rebel developments ltd. max claim harold price creek …
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R E B E L DEVELOPMENTS LTD.
MAX CLAIM
Harold P r i c e C r e e k Area , Omineca Mining Division,
Br i t i sh Columbia
NTS: 93M/6E
Approx. 55O16'; 127°101
REPORT ON EXPLORATION WORK J U L Y 1978
August 31st , 1978
1-425 HOWE STREET, VANCOUVER, B.C. V6C 2A9 TELEPHONE (604) 684-5433
TABLE O F CONTENTS
Page
1
3
INTRODUCTION
LOCATION AND ACCESS
. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .
PHYSIOGRAPHY ........................................ PROPERTY AND OWNERSHIP . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1978 WORK PROGRAM .................................. GEOLOGY ..............................................
Regional Geology . . . . . . . . . . .. . . . . . . . . . . . . .. . . . . . Local Geology . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . Mineralization . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . Details of Road Sections . . . . . . . . . . . . . . . . . . . . . . . . .
DISCUSSION ............................................ CONCLUSIONS . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . RECOMMENDATION . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . CERTIFICATE - J.B. P. Sawyer, P. Eng. . . . . . . . . . . . . . . . . . CERTIFICATE - T.B. Smar t , M. Sc. . . . . . . . . . . . . . . . . . . . . . LIST O F REFERENCES . .. . . . . . . . .. . . . . . . .. . . . . . . .. . . . . . APPENDIX A - Assay Cert i f icates
APPENDIX B - Petrographic Descriptions
APPENDIX C - Diamond Dr i l l Log EM-1, Graphical Ver t ica l A P P E N D I X D - Statement of Costs , Labour, etc. Section
Lis t of I l lustrations
F igure 1 - Genera l Location Sketch
F igu re 2 - Location Map, Hazelton A r e a
F igu re 3 - Prope r ty Map
F igure 4 - Regional Geology, Hazelton A r e a - 1'' = 10 mi.
Map 1 - Geological P l an
Map 2 - Sections 150N, 300N, 450N 1" = 200'
Map 3 - Sections 400S, 200S, Baseline 1'' = 200'
Map 4 - Sections 600N, 900N, 1200N 1" = 200'
1" = 200'
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14
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in pocket (1)
(i)
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in pocket (2)
in pocket ( 3 ) 1 1 II 1 1
I I I t I f
MAX CLAIM PROSPECT HAROLD PRICE CREEK
OMINECA MINING DIVISION, B. C.
G E N E R A L L O C A T I O N SKETCH e
Figure 1 S C A L E . I " = 125 MILES
1
INTRODUCTION
The Max Claim property of Rebel Developments Ltd. cons is t s of a total of 7 c la ims comprising 62 units acquired by option and by staking in the period October 1977 to la te January 1978. Sawyer Consultants Inc. of Vancouver was retained in November 1977 to supervise an exploration work p rogram on this property, and in the per iod November 20th to Dec- ember 12th, 1977, and January 5th to January 23rd, 1978, work c a r r i e d out included staking, construction of an access road f r o m Harold P r i c e Creek to the main showing a r e a , t r ac to r trenching and sampling, and diamond drilling. iently encouraging to justify a continued exploration program. prepared by Sawyer Consultants Inc. in Februa ry 1978 and revised a t the request of the management of Rebel Developments Ltd. in May 1978 descr ibed the resu l t s of the initial work program, and recommended a fur ther exploration program. The recommended p rogram was carefully planned to provide specific information on par t icular fea tures of the proper ty and an important aspect of the recommended p rogram was that the work should be c a r r i e d out in a logical t ime sequence. The p rogram visualized an initial work stage which would involve, principally, geological mapping and fur ther geochemical and geophysical work to a s s i s t in evaluating the potential for volcanogenic and/or bedded deposits, a s opposed to the gash vein type of mineralization in the intrusive rocks exposed in the December 1977 trenching, and did not include drilling as pa r t of the initial program.
The resu l t s of that initial work were considered suffic- The repor t
The work p rogram was commenced in ea r ly July 1978 with the geological work being c a r r i e d out by Mr. T. B. Smar t , M. Sc., a geologist working under contract to Sawyer Consultants Inc., and under the general supervision of the wri ter . Fa i r ly detailed geological work over a limited a r e a of the property was completed by Mr. Smar t and is descr ibed in the appropriate section of this report . The only other work completed in this p rogram was a par t ia l line cutting p rogram originally intended to provide control for geochemical and geophysical work. Developments Ltd. management, no additional geochemical o r geophysical work was attempted. dr i l l equipment. p rog ram and in the opinion on the Consultants i s of l i t t le consequence with respec t to the overal l geological program. expressed des i r e s of management to c a r r y out some physical work of this kind by personnel hired by Rebel Developments Ltd. expressly for this purpose. In late July the field exploration p rogram was suspended and a l l camp and equipment was removed f r o m the property on the sole decision of the management of Rebel Developments Ltd. brief field p rogram conducted during July has served to provide a m o r e detailed picture of the geology but has done nothing to contribute to our knowledge of the potential for economically viable mineralization within the sedimentary-volcanic sequence. ibility that such might occur.
On the decision of the Rebel
In addition, one dr i l l hole was put down using portable This d r i l l hole was not a pa r t of the originally recommended
The hole was dril led to meet
The work completed in the
Certainly it has not eliminated the poss -
3
LOCATION AND ACCESS
The property l ies a t and to the south of the junction of the Suskwa River and Harold P r i c e Creek, within the a r e a of NTS Quadrangle 93 M/6, in the Omineca Mining Division of Bri t ish Columbia. approximately 18 mi l e s east-northeast in a straight line f r o m the village of Hazelton, B. C. , and approximately 25 miles by road f r o m that point. Easy access to the proper ty may be had by t ruck using Highway #16 f r o m Hazelton o r Smithers to the Suskwa River F o r e s t r y Road, thence via this road to the 10.5 mile m a r k , and f r o m there by a bush road, which would be passable only to four-wheel dr ive vehicles during pa r t s of the yea r , a distance of approximately 7. 5 miles to the Suskwa River where there had former ly been a bridge. A t r a i l leads a c r o s s the Suskwa River and Harold P r i c e Creeks to the north boundary of the property, a distance of approxi- mately one-half mile. The road constructed in December 1977, leads f r o m Harold P r i c e Creek in a general southerly direction to the 2600 foot elevation on the north face of Blunt Mountain, a distance of approximately 6400 feet , involving a r i s e in elevation f r o m the r ive r of approximately 1000 feet.
The c la ims are
Alternatively, access may be had via char te red helicopter f r o m Smithers , which i s serviced by a permanent base of Okanagan Helicopters Ltd. An old, but secure , helicopter pad exists on the side of the mountain near the main showings and a new pad was built in July 1978 on the edge of the main t rench a rea .
PHYSIOGRAPHY
The a r e a i s one of marked relief and is well forested with mixed evergreen and coniferous - spruce, pine, cedar , e tc . , and deciduous - birch, poplar, e tc . , t rees . Some of these t r e e s a r e of a considerable s ize and would provide ample lumber fo r any mining o r construction required on the property.
Relief on the property var ies f r o m about 1600 feet (485 m e t r e s ) along Harold P r i c e Creek to about 4500 feet (1350 m e t r e s ) on Blunt Mountain on the southern end of the claims. P a r t s of the north face of the mountain on which the property l ies are quite s teep and in places , along some of the c reeks and higher on the mountain, locally precipitous. The property i s drained by seve ra l c r eeks which locally have cut quite s teep gullies, a s well a s s eve ra l sma l l e r seasonal drainages. feet long l ies in a saddle between the 3600 and 3700 foot elevations in the southwestern quadrant of the property.
A smal l lake approximately 1500
4
PROPERTY AND OWNERSHIP
The Max claim, comprised of six units, was staked and recorded in the name of John Young of Vancouver on September 9th, 1975. record number of this c l a im is 122. Beneficial ownership of this c la im i s divided between John Young and Maxwell Martin each a s to 2570, and Georgia Resources Ltd., a private company, a s to 50%. ments Ltd. by an agreement dated Nov. 3/77 and an amendment dated Nov. 17/77 acquired the option to purchase title and production rights to the property. The details of the t e r m s of this agreement are beyond the scope of this report .
The
Rebel Develop-
In November 1977, nineteen additional units in three separate claims named Martin #1, Martin #2, and Martin #3 were staked by S . J. Young a s agent for Rebel Developments Ltd. These three claims, having Record Nos. 850-852 inclusive, were recorded in Smithers on November 24th, 1977.
In the period January 17th to January Zls t , 1978, three additional c la ims, Martin #4, Martin #5, Martin #6, comprising a total of 37 units, and having Record Nos. 884-886 inclusive were staked by S. J. Young a s agent for Armand Arsenault. recording office of the B. C. Department of Mines on Februa ry 3rd, 1978, and were t r ans fe r r ed f r o m Mr. Arsenault to Rebel Developments Ltd. by a Bill of Sale recorded with the B.C. Department of Mines on Februa ry 17th, 1978, and acknowledged by B. C. Department of Mines receipt number 1172033.
These claims were recorded a t the Vancouver
The property now consists therefore of seven claims, Max, and Martin # 1 to #6 inclusive, comprising a total of 62 units, a l l of which a r e contiguous and l ie a t and about the junction of the Suskwa River and Harold P r i c e Creek in the Omineca Mining Division of Bri t ish Columbia. These claims a r e shown on B. C. c la im maps 93M/6E and 93M/3E.
All of this information is summarized in the following table and a plot of all of these claims is included a s F igure 3 of this report .
Tag No. of Record Expiry Claim Claim - No. Units Staked Recorded No. Date Map Ref.
Max 10399 6 Sept.7-8/75 Sept. 9/75 Martin #1 34639 3 Nov. 22/77 Nov. 24/77 Martin # 2 34640 10 Nov. 22/77 Nov. 24/77 Mart in #3 34641 6 Nov. 23/77 Nov. 24/77 Martin #4 34612 5 Jan. 20/78 Feb. 3/78 Martin #5 34613 12 Jan. 21/78 Feb. 3/78 Martin #6 34614 20 Jan, 18/78 Feb. 3/78
Total 62 Units
122 Sept. 9 /80 93M/6E 850 Nov. 24/78 93M/6E 851 Nov. 24/78 93M/6E 852 Nov. 24/78 93M/6E 884 Feb. 3/79 93M/6E 885 Feb. 3/79 93M/6E 886 Feb. 3/79 93M/6E &
93M/3E
REBEL DEVELOPMENTS LTD. MAX CLAIM PROSPECT AREA HAROLD PRICE CREEK OMINECA M.D.
British Columbia
PROPERTY MAP Scale: I : 50, 000 FIGURE: 3
6
The t e r m s of the option agreement between Georgia Resources Ltd. and Rebel Developments Ltd. provided that in the event the Agreement was abandoned the Max Claim and all of the contiguous c la ims staked by Rebel Developments Ltd. within a defined radius would r eve r t to Georgia Resources Ltd. It fur ther provided that all work completed on the c la ims was to be filed for a s ses smen t c red i t to Georgia by Rebel Developments Ltd. compliance with these provisions and af ter consultation with the principals of Georgia Resources Ltd. i t has been decided to consolidate the Max Proper ty into a single 40 unit Group. pertaining to c la im tenure under the Modified Grid System of Staking in B. C. allows reduction in the number of units in a c la im upon approval of the Gold Commissioner. In o rde r to achieve the above descr ibed consolidation it i s necessary to reduce the number of units in the Martin #5 Claim f rom 12 to 6, and in the Martin #6 Claim f r o m 20 to 4. been filed with the Gold Commissioner for the Omineca Mining Division in Smithers and Statement of Exploration & Development fo rms covering all of the work done on the Max and Martin Claims in the period November 1977 to August 1978 will be filed as soon a s possible. The amount of work completed should provide sufficient c red i t for at l eas t 488 uni t /years , i. e. sufficient to hold the proposed 40 unit Max Group for s eve ra l years .
In
Recent changes in the Regulations
Applications to effect this have
1978 WORK PROGRAM
The recommended work p rogram for 1978 included line cutting to es tabl ish control for geophysical (magnetometer and E. M. ) surveys , and geochemical soil sampling, geological mapping, to be followed by trenching and sampling, and a l imited amount of Winkie o r Packsac dril l ing p r e - para tory to a major drilling p rogram on any ta rge ts developed by the geo- logical, geophysical, and geochemical work. The f i r s t pr ior i ty was to be given to geological work to provide m o r e detailed information on the distribution of mineralization and i ts controls.
The actual work completed before the field work was suspended included :
1. Line cutting: - completion of only a par t ia l g r id consisting of a base line 3400 feet long, oriented 065O, and 5 gr id l ines for a total of 6300 feet, on the northwest side of the base line only. No l ines were cut on the southeastern side of the base line.
2. Geological mapping by T. B. Smar t , geologist. The mapping was begun in the a r e a of the main trenches excavated in December 1977 and January 1978, and was being extended to the a r e a s underlain predominantly by the sedimentary-volcanic sequences to the north, east , and southeast,
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7
when the program was halted. chip samples were collected f r o m exposures of sedimentary and/or volcanic rock which c a r r y finely disseminated sulphide mineralization. twelve samples f r o m seven locations were taken and these were submitted to Bondar-Clegg & Co. Ltd. in Vancouver for a s say for content of gold, s i lver , lead, zinc, and antimony. The samples were deliberately taken over fa i r ly large lengths in o rde r that the a s says would be a fair indication of the tenor of this type of mineralization.
A s par t of the geological evaluation seve ra l
A total of
3 . At the request of management, one Winkie d r i l l hole, designated EM-1, was dr i l led to a depth of 171 feet, near outcrop M-14 in the January 1978 t rench in which two beds of mass ive mineralization had been exposed. The hole was col lared below these beds and dr i l led vertically. intended to provide geological infor mat ion regarding the sedimentary /volcanic sequence below the exposed mineralized beds, and to determine if other mineral ized beds occurred. A log of the core f r o m this hole, and a ver t ica l section showing the formations intersected, accompany this report . Winkie d r i l l holes planned for a later stage to provide geological information in the area of the oxidized minera l showing a t location M-5, and in the a r e a of ea r l i e r defined (1968) geochemical anomalies, were not drilled.
It was
Other
GEOLOGY
Regional Geology
The regional geology of the c la im a r e a i s shown on G. S. C. Map 971A which indicates the genera l a r e a to be underlain by sediments, with some interbedded volcanic members , of upper Ju ras s i c to Cretaceous age, with middle o r upper Ju ras s i c age intermediate volcanics underlying the a r e a eas t of the property. Blunt Mountain itself is a Cretaceous intrusion of diorit ic composition which cuts the sedimentary and volcanic rocks.
More recent work in the general a r e a has refined this picture somewhat although no good recent geological map covering the a r e a has been published. mentary rocks in this a r e a a s being middle to upper Ju ras s i c (Bathonian to Oxfordian) of the Bowser Lake Group. shown on the ea r l i e r map, 971A, as being predominantly volcanic rocks of middle o r upper Ju ras s i c age with minor argi l l i te (Map Unit 12 ) a r e now shown a s being lower Cretaceous to Eocene Skeena and Sustut Group rocks. The Skeena Group i s descr ibed as comprising "interbedded mar ine and non- mar ine sedimentary and volcanic s t ra ta . sandstone, shale, and conglomerate with common minor o r major coal seams. Volcanics a r e g rey to green o r varicoloured basalt ic to rhyolitic brecc ias , tuffs, and flows. the group var ies f r o m place to place. I ' The Sustut Group, according to
Work by Tipper and Richards (1976) has defined the sedi-
The rocks immediately to the eas t
The sediments a r e greywacke,
The proportion of volcanics to sediments in
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Tipper and Richards (1976), is the youngest regionally significant sediment- a r y assemblage in the region which was ea r l i e r descr ibed by Lord (1948) a s Ira thick assemblage of conspicuously bedded and banded continental s t ra ta of relatively simple s t ructure . I ' Later workers , par t icular ly Eis- bacher (1974a), has sub-divided the group into a lower Tango Creek formation and an upper Brothers Peak formation which in turn have been sub-divided into seve ra l members . The sedimentary rocks of the Bowser Lake Group, which were deposited in the Bowser Basin, a successor basin to the volcanogenic Hazelton trough, are par t of the younger facies assembl- age of this group. commenced in Callovian (late middle Ju ras s i c ) time. La ter local vulcanism occurred along the margin of the basin. norther ly t ransport direction into this basin f r o m the Skeena Arch, and a southwesterly t ranspor t direction f r o m the Pinchi Belt. Tipper and Richards (1976) note that "the youngest s t r a t a of the Bowser Lake Group a r e mar ine and non-marine deltaic facies assemblages that underlie most of the southern Bowser Basin. Alluvial, shoreline and shallow mar ine facies of conglomerate, sandstone, si l tstone, and mudstone dominate, with fine grained sil tstone- shale-limestone dis ta l o r delta slope facies found locally on Blunt Mountain and Mount Thomlinson. adjacent a r e a s appear to fit this description.
They represent a fur ther mar ine regress ion which
Palaeocurrent data indicates a
Many of the rocks noted on the Max Claim and
There appears to be little recent detailed information about the economic geology of the a rea . known to host many minera l showings, predominantly of vein type which a r e frequently character ized by relatively high precious meta l values. a l so appears to be a prominent constituent in many of the known showings in the immediate a r e a of the Max Claims. appear not to have been well known nor extensively explored in the past.
The Smithers-Hazelton a r e a in genera l is
Antimony
The Max Claim showings themselves
Local Geology
The immediate a r e a of the present Max Claims was mapped in some detail during the 1960's by personnel attached to the Vancouver office of a major international mining company. In July 1978 additional mapping was c a r r i e d out by Mr. T. B. Smar t for Sawyer Consultants Inc. a s pa r t of the planned initial phase work p rogram recommended in the Februa ry 1978 repor t p repared by Sawyer Consultants Inc. a broad base for the m o r e detailed recent work. are provided by T. B. Smart.
The e a r l i e r mapping provided The following descriptions
The g,eological formations in the mapping a r e a a r e a s follows:
1. A sedimentary unit, r e f e r r ed to a s the Bowser Group sediments, which include quartzi tes , conglomerates, cher t s , sandstones, g r i t s , s i l t - stones, greywacke, shale and argil l i te, - a deltaic s e r i e s .
10
These a r e of middle and upper Ju ras s i c age, (Tipper & Richards 197 6).
2. An intrusive quartz-diorite with associated microdior i te and aplite dykes, of Cretaceous age.
The northwest par t of the mapping a r e a i s underlain by the quartz- diorite intrusive which has a steeply dipping contact with the sediments. The m o r e argil laceous components of the sedimentary sequence have been metamorphosed to a garnet-biotite hornfels and contain chiastolite a t some horizons. diorite contact to a distance of about 800 feet.
This contact aureole of a l te red rocks extends out f r o m the quar tz -
The sequence of rocks adjacent to the diorite intrusive includes both sedimentary members , quartzi tes , conglomerates etc. and apparently interbedded rocks which f r o m visual inspection and field relationships a r e thought to be volcanic. rocks ass ign a probable intrusive origin to them, but it is to be borne in mind that the petrographers did not have the benefit of the field observations. At this point a volcanic (or a t mos t a minor intrusive) origin of these m e m b e r s is favoured. be required to resolve this point.
The petrographic descr ipt ions of some of these
More extensive mapping and petrographic work will
Information f r o m mapping, and supported by data f r o m the EM-1 in an E N E 0 dr i l l hole, indicates that the sediments a r e dipping a t about 17
direction as shown in section 800N of baseline. Local dip measurements f r o m outcrops where bedding is indicated show a f a i r amount of variation so that the formations a r e locally folded while the s t r ike is generally N-S o r NNE-SSW. The rock sections exposed in the road and the mineral ized sections of the main trench, and by the c reek , show strong shearing and fair ly strong local crumpling of the beds. Jointing is strongly developed and the rocks presumably faulted locally, though the low percentage of out- c rop prevents m o r e positive information on the la t ter . nor ther ly dip is seen in the main t rench where quartzite is brought against ho rnf e l s .
One fault with a
Mineralization
The lead, zinc, antimony sulphide mineralization which has been seen to replace bedding and occupy f rac ture zones, especially in the upper quartzite horizon is most probably related to the quartz-diorite intrusion,
Information obtained f r o m the EM- 1 d r i l l core , however, indicates that some disseminated sulphide mineralization in the sediments may be of syngenetic origin o r possibly related to a distant volcanic source. quartzite horizon between 127. 0 and 152. 0 feet contains disseminations and impregnations of s ulphide .
The
11
c No mass ive sulphide mineralization was encountered in dr i l l hole EM-1 which was col lared a t the c reek below the mass ive sulphide replace- ment beds in quartzite. However, as no other holes were dril led, either a t a lower horizon (M-5-77 stibnite-sphalerite minera l showing) or a higher horizon (to tes t the c r e e k mass ive sulphide replacement bed in quartzite - t rench occurrence) the possibility of m o r e extensive, bedded, economic mineralization cannot be entirely eliminated. Also, the electromagnetic survey c a r r i e d out by the previous company would not necessar i ly take into account a flat-lying (bedded o r replacement) deposit, as encountered in the t rench - c reek quartzite horizon.
Details of Road Sections
Construction of the access road to the main t rench a r e a in December 1977 exposed seve ra l sections of outcrop along the road cut. been mapped in m o r e detail and a r e descr ibed as follows:
These have
M- 14A-77
A 6" band of mass ive sulphide mainly of sphalerite, galena and pyrite runs para l le l to the bedding within a light grey quartzite. It is vuggy in places and lies beneath an oxidation zone of i ron oxides, orange antimony oxide and a yellow arsenic-bear ing sulpho-salt, etc. contains disseminated pyrite beneath the vein. Below, a bluish-black quartzite contains l a rge r pyrite c rys ta l s and blebs. is of cher t . The above constitutes about 30 feet of the west end of the section. The cent ra l 3 0 feet consists of a sma l l open folded a r e a with lenses of yellow pyrite t calcite intercalated with the quartzite. 40 feet is a l a rge r fold within well-jointed quartzi te , and outlines a n i r - regular sphalerite-pyrite vein up to 6" wide.
The light g rey quartzi te
The floor of the c r e e k
The eas t e rn
M-6-77
The section shows fractured and well-jointed quartzi te and horn- 0 0 fe ls ic rocks dipping a t about 55
amounts of disseminated sulphide. cuts hornfels. A zone of f rac ture occurs a t the eas t end of the section with an eas te r ly dip and a steeply inclined shear zone near the aplite dyke dips west. Adjoining the section a t the west end is a sulphide-bearing quartzi te which can be t raced up the s t r e a m and adjoining a r e a and is ve ry probably the same horizon intersected in d r i l l hole EM-1 f r o m 127. 0 feet to 152, 0 feet.
to 60 E in some bands with moderate An aplite dyke dipping a t about 7OoW
M- 1-77
This section i s mainly of darkish well-jointed hornfelsic rock which appears to be dipping west a t about 45 to 50°. occurs within these rocks which a r e gently folded on E - W axes and f rac tured in places. A silicified greywacke with disseminated sulphide occurs a t the north end of the section.
0 A horizontal shear zone
12
M-10-77
In this section a nar row sphalerite-pyrite vein with bordering 0 0
oxidation mater ia l dips 65 , S60 E a t the contact of sheared and fractured greywacke and hornfelsic rock. The la t te r two rock types contain a moderate amount of disseminated sulphide adjoining the vein for s eve ra l feet.
M-15-77
The section is mainly of quartz-conglomerate and grit. The rocks a r e well-jointed and contain some shea r zones and f rac ture planes and exhibits minor folding. fine disseminated pyrite and is speckled with rusty spots.
One band of crumbly gr i t contains considerable
As reported above, a number of chip samples were collected f r o m seven outcrop exposures, generally over widths of s eve ra l feet. All of the samples re turned generally low values in base and precious metals. bes t sample #13587 taken over fourteen feet a t location M-10-77N returned 0. 006 oz. /ton gold and 0. 03 oz. /ton silver. a r e given in the following table (page 13).
The
The details of these samples
Some tungsten mineralization has been reported f r o m the property. Mr. Arsenault repor t s that an ultraviolet lamp when used on the exposed sur faces of the main t rench a t night revea l extensive light bluish fluorescense s imi la r to that due to scheelite. office revealed a small amount of s imi la r f luorescence and one sample submitted to Bondar-Clegg & Co. Ltd. re turned an a s say of 0. 03% tungsten. This resu l t is a l i t t le surpr i s ing in view of the ve ry sma l l a r e a of minera l - ization evident f r o m the fluorescence.
A few hand specimens examined in the
All of the core f r o m the drilling c a r r i e d out in January 1978 was lamped by the wr i t e r a t the t ime the core was logged, and no significant f luorescence was noted. Similarly a number of hand specimens collected f rom field work in December 1977,and January 1978, and in July 1978, have a l s o been checked for tungsten mineralization and none has been detected. Although no la rge o r economically significant amounts of scheeli te o r other tungsten mineralization have been detected to date, any continuing p rogram should include thorough testing for this mineral .
A s s a y S a m p l e T a g S e c t i o n Leng th No. (ft. )
13585 M- 1-77 30
13584 M-3A 12
13583 M-5-77 16
13579 M - 6-77A 2 0 96 13580 M-6-77B 10 13581 M-6-77C 8 13582 M-6-77D 4
13586 M - 10 - 7 7 s 6 96 13587 M-10-77N 14
13577 M-11-77A 4 ::: 13578 M- 11-77B 5
13576 M-15-78 16 - ~~
ASSAY RESULTS
A u A g Sb P b ZTl
4 0.002 0.02 4 0 . 0 1 0 .01 0 . 0 2
c 0.002 4 0 .02 40. 0 1 0 .02 0 .02
40 .002 0. 03 4 0 . 0 1 0 .02 0. 03
40. 002 3. 02 4 0 . 0 1 0. 02 0 .02 4 0 . 002 c 0.02 4 0 . 0 1 0 .01 0 . 0 1 c o . 0 0 2 0.02 4 0 . 0 1 0 . 0 1 0 . 0 1 40. 002 0. 03 4 0 . 0 1 0. 02 0 . 0 1
40 .002 0. 03 40.01 0.01 0 .02 0 .006 0. 03 40 ,Ol 0 . 0 1 0 .06
c o . 0 0 2 0. 02 4 0 . 0 1 0 .01 0 .02 c o . 0 0 2 0. 03 4 0 . 0 1 0. 03 0. 04
4 0 .002 0. 02 4 0 . 0 1 0 . 0 1 0 .02
I
-I ~~ -~
14
DISCUSSION
The most spectacular metall ic mineralization on the property is that discovered by the t r ac to r trenching work in December 1977 below the original hand dug t renches put down by prospectors in the la te 1960's. The diamond drilling p rogram in January 1978 demonstrated conclusively that this mineralization, though spectacular and returning impressive values in s i lver , lead, zinc, antimony and some gold, is confined to gash veins in the intrusive diorite and is thus of ve ry limited extent with no potential for development a s a mineable deposit.
Trac tor trenching in January 1978, a t the t ime the dril l ing p rogram was in p rogres s , exposed interesting mass ive sulphide and sulpho-salt mineralization in quartzit ic sediments adjacent to the diorite intrusive. These occurrences were bedded near the contact and suggested the possibility of the existence in the a r e a of syngenetic and/or synvolcanic bedded deposits. At the point of exposure they were s t i l l essentially a t the contact with the intrusive, and the possibility remained that these were local replacement phenomena within the contact zone. the access road to the main t rench area in December 1977, two other oxide zones were exposed along the road some 700 feet distant and 1,100 feet distant f r o m the then known mineralization, and these occurrences suggested that perhaps the bedded mineralization in the late t renches near the intrusive contact was m o r e extensive and that the new oxide zone exposures might be extensions of it. Style of mineralization and metal l ic content, specifically s i lver and antimony in the lower showing, and general attitude in the narrow upper showing, lent some support to this possibility, it being remembered that the ground was snow covered a t that time and no good exposures of geology were available other than in the trenched a r e a s . The p rogram recommended for 1978 accepted the fact that the main t rench mineralization was of no economic significance and was aimed specifically to attempt to build up a m o r e complete geological picture through mapping, geochemical and geophysical work. work would be completed before any g rea t amount of physical testing by trenching o r dril l ing was attempted. pleted has not eliminated the possibility that the bedded mineralization exposed in the t renches is m o r e extensive than immediately apparent and may in fact underlie a considerable pa r t of the northeastern Max Claim and adjacent Martin 1 Claim. may extend further west in the northern par t of the Max Claim and southern pa r t of Martin 5 Claim beyond the intrusive contact.
However in the course of constructing
The p rogram was s o planned that this phase of the
The l imited amount of mapping com-
In addition there is some possibility that this mineralization
Ea r ly in the July 1978 mapping p rogram management of Rebel Developments Ltd. expressed the des i r e to c a r r y out some drilling using portable dr i l l equipment. wr i t e r suggested that a hole located in the t rench near location M-14 and dr i l led vertically would supply some additional information about the volcanic
Solely to meet this request of management, this
15
sedimentary/sequence below what was exposed. below the exposed mineral ized beds thus the only information it could provide was whether o r not there were additional mineral ized horizons lower in the sequence. The hole was not considered to be of any grea t importance other than to provide a ve ry limited amount of local geological information. obviously could not provide any information about the la te ra l extent of the beds below which it was collared. have been put down near the lower mineralized showing (M-5 a r e a ) and further eas t along the road a t a location in which the Consultant had recom- mended that a hole be dril led with the big machine in January 1978. decision to cur ta i l the program a t the end of July 1978 was entirely a management decision. work p rogram has added little o r nothing to our pract ical knowledge of the mineralization on the Max prospect.
The hole was col lared
It
Subsequent portable dr i l l holes could
The
In the opinion of the Consultants the very limited 1978
CONCLUSIONS
Based on the descriptive data and discussion provided above, the following conclusions a r e drawn.
(1) Vein type mineralization within the intrusive rocks exposed by the December 1977 trenching, and fur ther tes ted by January 1978 drilling has no potential for development into a mining situation.
( 2 ) Significant amounts of disseminated and semi-mass ive sulphide and sulpho-salt mineralization occur in the mixed volcanic sedimentary assemblage which i s exposed in t renches immediately adjacent to the intrusive and which f r o m mapping is shown to underlie the a r e a to the east , northeast , and north of the intrusive on the Max and Martin # 5 Claims.
(3) There appear to be only two distinct bedded mi-neralized horizons, these being the two horizons exposed in the t rench a t locations M-14, M-14A, etc.
(4) The a r e a l extent of these relatively flat lying beds i s unknown but extends for a t least 1,000 feet to the eas t , and 1, 100 feet o r 1 , 2 0 0 feet to the north-northeast .
(5 ) The degree of disseminated mineralization in quartzit ic beds and in some other hornfelsic and/or volcanic horizons is probably anomalous in t e r m s of the overal l regional geology.
( 6 ) The limited amount of mapping completed suggests the possibility of local folding within the relatively flat lying beds and the possibility exists of thickening and/or concentration of sulphides by these s t ruc tura l events.
16
(7) Thin section descriptions of some of the rocks f r o m the January 1978 drilling, which descr ibes them as being hypabyssal equival- ents of the intrusive, are open to question on the basis of field observation. In the opinion of the Consultant, some of these rocks a t least a r e possibly, if not probably, of volcanic origin.
(8) The overal l resu l t s of work on the Max Cla im by Rebel Develop- ments Ltd. has not provided any strongly positive indications of economic concentrations of meta ls within the property boundaries nor has it eliminated the possibility that such do exis t on the property.
RECOMMENDATION
In o rde r to investigate the mine ra l occurrences on the Max Proper ty m o r e fully so that a proper evaluation of the potential of the property can be made the work p rogram recommended earlier should be completed.
Re spec t f ully s ubmi t t ed ,
SAWYER CONSULTANTS INC.
T.B. Smart , M.Sc. Geologist
17
CERTIFICATE
I , J. B. P. Sawyer , DO HEREBY CERTIFY:
(1) That I am a consulting geologist with bus iness office a t 1 - 425 Howe S t r ee t , Vancouver, B. C. V6C 2A9, and P res iden t of Sawyer Consultants Inc.
( 2 ) That I am a graduate in geology of Manches te r University (B.Sc. - 1953) and of the University of Wes te rn Ontar io (M. SC. - 1.957).
(3) That I am a Regis te red P ro fes s iona l Engineer (geological) in the Associat ion of Profess iona l Engineers of the Province of Br i t i sh Columbia, and have non-resident s ta tus with the Associat ion of P ro fes s iona l Engineers of Manitoba,
(4) That I am a Fel low of the Geological Associat ion of Canada (1965), a Member of the Canadian Insti tute of Mining and Metallurgy (1960), and Fellow of the Geological Society of London (1978).
(5) That I have prac t iced m y profess ion as a geologist f o r the pas t twenty-four y e a r s .
(6) That the information, opinions and recommendat ions in the at tached r epor t a r e based on personal knowledge gained f r o m work on the Max proper ty in Dzcember 1977, and in the per iod January 10th to August l s t , 1978, on pe r sona l r e s e a r c h of published m a p s and r e p o r t s of the area, and d iscuss ions with other geological pe r sonne l who have worked in the area,
(7) That I own no in t e re s t in the s h a r e s o r s ecu r i t i e s of Rebe l Developments Ltd. nor of Georgia Resources Ltd. , no r do I expect to rece ive any such in te res t .
Dated a t Vancouver , Br i t i sh Columbia, this 31sk day of August, 1978.
18
CERTIFICATE
I, Thomas B. Smar t of Vancouver, B. C. , do hereby cer t i fy that:
(1) I am a geologist holding the degrees of B.Sc. (1956) and M. Sc. (1961) f r o m London University.
(2) That I have prac t i sed my profession as a geologist over the past twenty years .
( 3 ) That I own no interest in the s h a r e s o r securi t ies of Rebel Developments Ltd. and do not expect to receive any such interest .
T. B. Smart , M.Sc.
Dated a t Vancouver, B.C. this 31st day of August 1978.
19
LIST O F REFERENCES
Eisbacher , G. H. 1974a: Sedimentary and tectonic evoluation of the Sustut and Sifton basins , north-central Br i t i sh Columbia; Geol. Surv. Can. P a p e r 72-31.
1974b: Evolution of successo r basins in the Canadian Cordi l le ra ; in modern and ancient geosynclinal sedimentation, SOC. Econ. Paleontol. Mineral; Spec. Publ. No. 19.
Lord, C.S. 1948: McConnell C r e e k map area, C a s s i a r d i s t r ic t , Br i t i sh Columbia; Geol. Surv. Can. Mem. 251.
Rice, H.M.A. 1948: Map 971A, Smi the r s -For t St. J ames , Bri t ish Columbia.
Richards, T . A . 1974a: Hazelton eas t half (93M eas t half); in Report of Activit ies, Geol. Surv. Can. Pape r 74-1A, pt. A, p. 35-37.
1974b: Hazelton e a s t half (93M eas t ) ; Geol. Surv. Can. Open F i l e Report No. 215.
1978: Geology of Hazelton (west half) m a p a r e a , Br i t i sh Columbia, in Curren t Research , P a r t A , Geol. Surv. Can. P a p e r , pp. 59-60.
Richards, T.A. and Jeletzky, 0. L. 1975: A pre l iminary study of the Upper J u r a s s i c Bowser assemblage in the Hazelton wes t half m a p a r e a , Br i t i sh Columbia (93M-W1/2); in Report of Activit ies, P a r t A , Geol. Surv. Can., P a p e r 75-1A, p.31-36.
Taylor, D. P. 1977: P rope r ty Inspection and Geological Report on the Max Cla im, Harold P r i c e Creek , Omineca M. D., B. C. - repor t to proper ty owners dated Sept. loth, 1977.
Tipper, H. W. and Richards, T. A. 1976: J u r a s s i c Strat igraphy and History of North Cent ra l Br i t i sh Columbia; Geol. Surv. Can. Bull. 270.
A P P E N D I X "A
Bondar-Clegg & Company Ltd. A s s a y C e r t i f i c a t e s
TO: Sa, -r Consultants
MARKED
Section
R E B E L - M A ; J L A Z M
GOLD
Ounces Value per Ton m r Ton
PAGE No. 1 BONDAR-CLEGG & COMPANY LTD.
SILVER
Ounces per Ton
0.02
0.02
0.03 0.02
4.02 0.02
0.03
0.03
4.02
1 - 425 Howe Street Vancouver, B. C. V6C 2A9
Pb Zn Sb TOTAL VALUE PER TON
Percent Percent Percent Percent Percent Percent Percent (2000 m.1
0.01 0.02 4.01 Chip s;,mple a c r o s s 16' sectio:n Volcanic Cr.
0.01 0.02 ~0.01 Chip s;.mple over 49 section. 0.03 0.04 <0.01 Chip sample oyrer 5' w,.dth.
0.02 0.02 ~0.01 20' section sarnpled fr Dm fine-grained volcanic
0.01 0.01 0.01 0.01 <0.01 ~0.01 Sam$ V o l c t over r o c j a m p l e / e r 1 1 in da k volca 8 ' b g t h . ic rock,
0.02 0.01 ~0.01 Volca 'c rock sample v e r 4' ection.
0.02 0.03 <0.01 Volca 'c rock xposur at r o a side, 16' length. 0.02 0.02 4.01 Above Id dia ond dr i 1 pump relay.
-
rock.
I
Samples submitted: August 1, 1978 CERTIFICATE OF ASSAY Results completed: August 10, 1978
15' 13576 M-15-78
4' [ 13577 M-11-77A 5' ( 13578 M-l l -77B
20' 13579 M-6-77A
10' 13580 M-6-77B
8' 13581 M-6-77C
4' 13582 M-6-77D
16' 13583 M-5-77
12' 13584 M-3A
30' 13585 M-1-77
6' 13586 M-10-77(S)
14' 13587 M-10-77(N]
3 )It'lXbQ &ifE that the following are the results of assays made by us upon the herein described ore samples.
<o. 002 <0.002
~0.002
4.002
4.002
<0.002
<0.002
4.002
4. 002 4.002
4.002
0.006
0.02
0.03
0.03
0.02 4.01 30' le
0.02 4 - 0 1 0.06 ~0.01
0.01
0.01
0.01
r i
REPORT NO - ALQ - 593 To: . Jyer Consul tants I n c . REBEL A X C L A M RAGE No. 1 BONDAR-CLEW & COMPANY LTD. DATE: August 1 7 . 1978
GOLD MARKED
per Ounces Ton Dor Value Ton
#l - 425 Howe S t r e e t Vancouver, B . C . 'V6C 2A9
SILVER W TOTAL VALUE
PER TON per Ounces Ton Percent Percent Percent Percent Percent Percent Percent (2000 LBS.)
0.03 Grab sample f rom ma*h trench.
* ,TJ
cd
8 54 s; - -
CERTIFICATE OF ASSAY Samples Submitted: August 16, 1978 Results Completed: August 17, 1978
13562
n I-.
I-. Y
APPENDIX llB"
Vancouver Petrographics Ltd. - Petrographic Descriptions
r-------- -- --1
J A M E S V I N N E L L '\I I., r
JOHN G. P A Y N E I , i !) I c < ' 21,t
A P P E N D I X "B'l
P.O. BOX 39 8087 N A S H STREET FORT L A N G L E Y . R.C. V G X 1JG
PHONE (6041 5 3 3 i 1 5 5
1 5 J u l y , 1978
M r . Tom Smar t Swayer C o n s u l t a n t s I n c 1-425 H o w e S t r e e t Vancouver , B . C . V6C 2A9
Dear S i r :
sample numbers and i d e n t i f i c a t i o n s are as f o l l o w s : Enc losed are s e v e n p e t r o g r a p h i c d e s c r i p t i o n s . The
M-6-78 m o n z o n i t i c ( ? ) f e l s i t e M-15-78 d i o r i t i c ( ? ) f e l s i t e RM-1-78 (53 .5 ) d i o r i t e RV-1-78 ( 1 0 1 ) d i o r i t e IIM-3-78 ( 1 7 . 5 ) d i o r i t e ftvl-3-78 (109 .9 ) d i o r i t i c ( ? ) f e l s i t e RM-4-78 ( 5 6 ) d i o r i te
The t h i n s e c t i o n s a re e n c l o s e d w i t h t h e s e d e s c r i p t i o n s ; The re ject s l ices and samples f o l l o w u n d e r s e p a r a t e cover. P l e a s e d i r ec t e n q u i r i e s r e g a r d i n g t h e d e s c r i p t i o n s t o M.S. B l o o m , c/o Vancouver P e t r o g r a p h i c s .
The e n t i r e sample s u i t e i s a p p r o x i m a t e l y o f d i o r i t i c t o m o n z o n i t i c c o m p o s i t i o n , b a s e d upon t h e modal p e r c e n t a g e s o f q u a r t z and f e l d s p a r s , and t h e p l a g i o c l a s e c o m p o s i t i o n . The t e x t u r e s v a r y from e x c e e d i n g l y f i n e - g r a i n e d t o medium-grained and are t y p i c a l o f c h i l l e d m a r g i n s , border f a c e i s , a n d / o r o f f - s h o o t s o f l a r g e r p l u t o n s of p o s s i b l e g r a n o d i o r i t e c o m p o s i t i o n . More a c c u r a t e es t imates o f r o c k c o m p o s i t i o n w i l l r e q u i r e f e l d - s p a r s t a i n i n g i n the medium g r a i n e d va r i e t i e s , and whole r o c k c h e m i c a l a n a l y s e s i n t h e f i n e - g r a i n e d ( f e l s i t i c ) t e x t u r e s . The sample s u i t e i s a f f e c t e d by q u a r t z - s e r i c i t e and c a r b o n a t e a l t e r a t i o n o f v a r y i n y i n t e n s i t i e s , p resumably w i t h q u a r t z - s e r i c i t e a s t h e e a r l i e r s t a g e f o l l o w e d by c a r b o n a t e o v e r p r i n - t i n g .
Thank y o u f o r v s i n q o u r services.
Very t r u l y y o u r s ,
i,:p { )' -r I - _ _ _ _ Mark S. Bloom Vancouver P e t r o g r a p h i c s
Sample Number:
Mineralogy :
M-6-78 groundmas s 7 0 K-fe ldspar 17 p l a g i o c l a s e 6 q u a r t z 2 opaques 3 w h i t e mica /c l ay 2 c h l o r i t e t r z i r c o n t r
C l a s s i f i c a t i o n : monzon i t i c ( 2 ) f e l s i t e
F a b r i c and t e x t u r e : h o l o c r y s t a l l i n e , hypid iomorphic-granular
The f a b r i c o f t h i s r o c k g e n e r a l l y resembles t h a t of M-15- 7 8 , a l t h o u g h somewhat c o a r s e r - g r a i n e d . The pr imary c o n s t i t u - e n t s ( q u a r t z , K- fe ldspa r , p l a g i o c l a s e ) o c c u r i s a f i n e - g r a i n e d i n t e r l o c k i n g mosaic w i t h i r r e g u l a r g r a i n boundar i e s . Micro- p h e n o c r y s t s of q u a r t z , I<- fe ldspar and p l a g i o c l a s e are v i s i b l e i n t h e groundmass. There i s no d i s t i n c t i v e d i f f e r e n c e i n t h e g r a i n s i z e among t h e s e c o n s t i t u e n t s . Q u a r t z i s a n h e d r a l i n o u t l i n e , f i l l i n g i n t e r s t i c i e s among t h e f e l d s p a r s and ground- m a s s . The g r a i n b o u n d a r i e s are r e l a t i v e l y s h a r p . Undulatory e x t i n c t i o n i s n o t v i s i b l e . K-fe ldspar i s s u b h e d r a l i n o u t l i n e and may be a d j a c e n t t o p l a g i o c l a s e , q u a r t z , o r t h e groundmass. I t i s somewhat p e r t h i t i c , and myrmeki t ic t e x t u r e s are l o c a l l y v i s i b l e . P l a g i o c l a s e is g e n e r a l l y e u h e d r a l i n o u t l i n e , A l b i t e and combined c a r l s b a d - a l b i t e tw inn ing are c h a r a c t e r i s t i c . The p l a g i o c l a s e composi t ion i s c a l c i c a n d e s i n e ( A n 3 8 ) , de te rmined by t h e Michel-Levy t e c h n i q u e .
T h i s f e l s i t e i s i n c i p i e n t l y a l t e r e d t o w h i t e m i c a / c l a y s , c h l o r i t e , and opaques. The degree o f a l t e r a t i o n i s c o n s i d e r - a b l y less t h a t i n 5115-78. Very f i n e - g r a i n e d a g g r e g a t e s o f w h i t e m i c a and/or c l a y s a r e d i s t r i b u t e d th roughou t t h e s e c t i o n . T h i s a l t e r a t i o n a p p e a r s t o o r i g i n a t e i n t h e groundmass, and does n o t s i g n i f i c a n t l y a f f e c t t h e K-fe ldspar and p l a g i o c l a s e mic rophenocrys t s . C h l o r i t e i s a l s o s c a t t e r e d th roughou t , and i s o f t e n associated w i t h opaques. The opaques are g e n e r a l l y i r r e g u l a r i n o u t l i n e . S e v e r a l u n a l t e r e d g r a i n s of b i o t i t e a r e v i s i b l e a s s o c i a t e d w i t h t h e opaques. Carbonate i s n o t v i s i b l e i n s i g n i f i c a n t p r o p o r t i o n s . The opaques are presumed t o have
I i
I
I been i n t r o d u c e d d u r i n g t h e a l t e r a t i o n e v e n t .
A s i n M-15-78, t h e rock t e x t u r e s u g g e s t s i n t r u s i v e o r i g i n f o r this rock . A more r e l i a b l e estimate o f rock compos i t ion i s p o s s i b l e o w i n g t o the s l i g h t l y c o a r s e r g r a i n s i z e . The ap- proximate f e l d s p a r r a t i o and q u a r t z c o n t e n t s u g g e s t s d i o r i t i c t o monzoni t ic composi t ion .
f Sample Number:
Mineralogy:
M-15- 7 8
groundmas s q u a r t z opaques w h i t e m i c a c a r b o n a t e c h l o r i t e
74 2 3 6
1 4 1
C l a s s i f i c a t i o n : f e l s i t e
F a b r i c and t e x t u r e : h o l o c r y s t a l l i n e , hypdiomorphic-granular
t e r i z e s t h i s rock . The c o n s t i t u e n t s are presumed t o be q u a r t z and f e l d s p a r s ; however, i n d i v i d u a l g r a i n s are too minute f o r s a t i s f a c t o r y o p t i c a l r e s o l u t i o n and i d e n t i f i c a t i o n . The com- ponen t s o f t h e groundmass Dccur i n an i n t e r l o c k i n g mosaic w i t h v e r y i r r e g u l a r boundar i e s . Microphenocrys ts of q u a r t z and p l a - g i o c l a s e are v i s i b l e i n t h e groundmass. The d imens ions o f t h e q u a r t z exceed t h o s e o f t h e p l a g i o c l a s e by a fac tor o f approxi - ma te ly t e n . The q u a r t z i s g e n e r a l l y a n h e d r a l w i t h somewhat s u t u r e d g r a i n boundar i e s . T h i s may i n d i c a t e p a r t i a l r e s o r p t i o n during. c r y s t a l l i z a t i o n . Undula tory e x t i n c t i o n has n o t deve l - oped i n t h e q u a r t z g r a i n s . P l a g i o c l a s e mic rophenocrys t s are e u h e d r a l i n o u t l i n e and i n r e l a t i v e l y s h a r p c o n t a c t w i t h t h e groundmass. A l b i t e and combined c a r l s b a d - a l b i t e tw inn ing are t y p i c a l . The p l a g i o c l a s e compost ion, de t e rmined by t h e . Michel- Levy t e c h n i q u e , r a n g e s from calcic a n d e s i n e t o l a b r a d o r i t e (An38-54 ) . The p l a y i o c l a s e / K - f e l d s p a r r a t i o canno t a c c u r a t e l y e s t i m a t e d .
c h l o r i t e - p y r i t e . C e n t e r s o f a l t e r a t i o n a p p a r e n t l y o r i g i n a t e i n t h e groundmass. Randomly-oriented s h r e d s o f se r ic i te are su r rounded by c a r b o n a t e . These c lo t s are randomly d i s s e m i n a t e d th roughou t t h e s e c t i o n . Sh reds o f c h l o r i t e and c l o t s of an opaque ( p y r i t e ) are a l s o randomly s c a t t e r e d th roughou t t h e sec- t i o n . They do n o t appea r t o be s p a c i a l l y r e l a t e d t o t h e seri- c i t e - c a r b o n a t e a l t e r a t i o n . O c c a s i o n a l l y , t h e morphology o f t h e opaque resembles l a t h s of b i o t i t e , and i t i s a s s o c i a t e d w i t h c o a r s e r - g r a i n e d w h i t e m i c a and i r o n s t a i n i n g . T h i s sug- g e s t s comple te r ep lacemen t of f e rmer fe r romagnes ian microphe- n o c r y s t s by s e r i c i t e and s u l f i d e s . The opaques i n t h i s sec- t i o n have presumably been i n t r o d u c e d d u r i n g hydro thermal a l t e r - a t i o n .
The t e x t u r e of t h i s rock s u g g e s t s t h a t it i s i n t r u s i v e i n o r i q i n , pe rhaps an offshoot o r c h i l l e d margin o f a l a r g e r p lu- t o n . S e v e r a l l i n e s of ev idence s u p p o r t t h i s c o n c l u s i o n : 1) t h e homogeneous ( n o n - p o r p h y r i t i c ) n a t u r e o f t h e groundmass, and 2 ) the absence of f e a t u r e s t y p i c a l o f v o l c a n i c rocks such as bimodal g r a i n s i z e d i s t r i b u t i o n , f low-banding, and zones o f weld ing (glass). The mode of t h i s rock s u g g e s t s t h a t i t may be t h e f i n e - g r a i n e d c o u n t e r p a r t of a d i o r i t e t o g r a n o d i o r i t e .
An e x c e e d i n g l y f i n e - g r a i n e d , f e l s i t i c groundmass charac-
The f e l s i t e i s modera te ly a l t e r e d t o s e r i c i t e - c a r b o n a t e -
. Sample Number: RM-1-78(53.5)
Mineralogy: p l a g i o c l a s e 47 K-fe ldspar 18 q u a r t z 2 b i o t i t e 6 sphene 1 w h i t e mica /c l ay 13 c a r b o n a t e 1 2 opaques 1 z i r c o n , a p a t i t e t r
C l a s s i f i c a t i o n : d i o r i t e
Fabric and t e x t u r e : medium-grained, e q u i g r a n u l a r h o l o c r y s t a l l i n e , hypid iomorphic-granular
Plagioclase i s t h e pr imary c o n s t i t u e n t . I t is e u h e d r a l t o s u b h e d r a l , o c c u r r i n g i n an i n t e r l o c k i n g mosaic o f randomly or- i e n t e d l a t h s . The p l a g i o c l a s e i s i n t e n s e l y a l t e r e d ; however, o c c a s i o n a l u n a l t e r e d g r a i n s o r p o r t i o n s of g r a i n s show a l b i t e twinning . The compos i t ion , de t e rmined by t h e Michel-Levy t ech - n i q u e , i s a n d e s i n e ( A n 3 4 ) . Two a l t e r a t i o n t y p e s are v i s i b l e . The ea r l i e s t c o n s i s t s o f n e a r l y complete r ep lacemen t o f p l a g i o - clase by w h i t e mica /c l ays . Sh reds o f w h i t e mica are f r e q u e n t , b u t t h e c l a y a p p e a r s predominate . O u t l i n e s o f former p l a g i o - clase are v i s i b l e , b u t t h e i n t e r i o r s of t h e f e l d s p a r i s coated w i t h r a d i a t i n g masses o f low b i r e f r i n g e n c e . La te r c a r b o n a t e has been i n t r o d u c e d , p a r t i c u l a r l y a l o n g t h e margins and’ a l o n g c l e a v a g e traces and f r a c t u r e s .
K- fe ldspa r i s a n h e d r a l i n o u t l i n e , f i l l i n g i n t e r s t i c i e s among t h e p l a g i o c l a s e l a t h s . I t is i n t i m a t e l y a s s o c i a t e d w i t h a n h e d r a l q u a r t z , c r y s t a l l i z i n g approx ima te ly s i m u l t a n e o u s l y . The K-fe ldspar i s n o t p e r t h i c and i s untwinned. I t remains f r e s h a f t e r b o t h p e r i o d s of a l t e r a t i o n .
Euhedra l t o s u b h e d r a l b i o t i t e f i l l s i n t e r s t i c i e s among p l a g i o c l a s e l a t h s , and w a s fo l lowed by K-fe ldspar and q u a r t z . I t i s p e r v a s i v e l y a l tered t o w h i t e m i c a and c a r b o n a t e . The w h i t e mica a l t e r a t i o n a p p e a r s t o i n i t i a l l y r e p l a c e t h e b i o t i t e , and i s i n t u r n r e p l a c e d by t h e c a r b o n a t e . N o u n a l t e r e d b i o t i t e remains . Most o f t h e w h i t e m i c a a l t e r a t i o n i s f i n e - g r a i n e d and a s s o c i a t e d w i t h q u a r t z . Occas iona l c o a r s e - g r a i n e d seri- c i t e i s v i s i b l e . R e l a t i v e l y h i g h p r o p o r t i o n s o f sphene were a s s o c i a t e d w i t h t h e b i o t i t e , as i n RM-4-78. Zi rcon , a p a t i t e , and opaques a r e randomly d i s s e m i n a t e d th roughou t t h e s e c t i o n . T h i s rock i s d i o r i t i c i n composi t ion .
Sample Number:
Mineralogy:
RM-1-78 (101)
p l a g i o c l a s e 5 4 K- f e l d s p a r 18 q u a r t z 2 b i o t i t e 7 w h i t e m i c a 1 c h l o r i t e 3 c a r b o n a t e 1 2 opaques 3 z i r c o n , a p a t i t e t r
C l a s s i f i c a t i o n : d i o r i t e
F a b r i c and t e x t u r e : medium g r a i n e d , e q u i g r a n u l a r , holo- c r y s t a l l i n e , hypid iomorphic-granular
Euhedra l t o s u b h e d r a l p l a g i o c l a s e i s t h e p r imary c o n s t i - t u e n t . The l a t h s show a l b i t e and combined c a r l s b a d - a l b i t e tw inn ing . The p l a g i o c l a s e compos i t ion , a n d e s i n e (An been de te rmined by t h e Michel-Levy t e c h n i q u e . N o r m a zoning i s p r e s e n t . The p l a g i o c l a s e i s p a r t i a l l y a l t e r e d t o mosaics o f c loudy c a r b o n a t e and s h r e d s o f w h i t e mica. The d e g r e e of a l t e r a t i o n i s minor .
I<-Eeldspar i s s u b h e d r a l t o a n h e d r a l i n o u t l i n e . I t oc- c u r s i n t e r s t i t i a l l y among l a t h s o f p l a g i o c l a s e . The K-feld- s p a r i s untwinned and n o n - p e r t h i t i c . I t i s also g e n e r a l l y u n a l t e r e d . I t i s d i s t i n g u i s a b l e from q u a r t z o n l y by t h e in- t e r f e r e n c e f i g u r e and r e l i e f . Q u a r t z i s a n h e d r a l and o c c u r s i n t e r s t i t i a l l y among t h e f e l d s p a r s . Myrmekitic q u a r t z - f e l d - s p a r t e x t u r e s are n o t v i s i b l e .
o c c u r r i n g i n t e r s t i t i a l l y among t h e p l a g i o c l a s e l a t h s and i s d i s t i n c t i v e l y ea r l i e r t h a n t h e K-fe ldspar and q u a r t z . I t i s a s s o c i a t e d w i t h i n c l u s i o n s o f opaques , q u a r t z , a p a t i t e , and z i r c o n . The b i o t i t e i s v a r i a b l y a l t e r e d t o c h l o r i t e , carbo- n a t e , and w h i t e m i c a . The c h l o r i t e / w h i t e m i c a a l t e r a t i o n i s ear l ier and o v e r p r i n t e d by c a r b o n a t e . The ea r l i e r a l t e r a t i o n e v e n t i s v i s i b l e i n a l l t h e b i o t i t e and o c c u r s as r ep lacemen t p a r a l l e l t o t h e c l e a v a g e traces. I t is a s s o c i a t e d w i t h f i n e - g r a i n e d opaques. The l a te r c a r b o n a t e a l t e r a t i o n comple t e ly r e p l a c e s b i o t i t e in a p o r t i o n o f t h e s e c t i o n , and o n l y i n c i - p i e n t l y r e p l a c e s b i o t i e i n t h e o t h e r p o r t l o n . T h i s i s v i s i b l e i n hand specimen as a d i s t i n c t i o n i n c o l o u r . The d a r k e r por- t i o n c o n t a i n s a g r e a t e r p r o p o r t i o n o f u n a l t e r e d b i o t i t e . C r o s s - c u t t i n g t h i s p o r t i o n o f t h e s e c t i o n i s a c a r b o n a t e v e i n a round which a l l t h e maf i c are r e p l a c e by c a r b o n a t e . Fine- g r a i n e d d i s s e m i n a t e d c h l o r i t e and opaques are a l so p r e s e n t t h r o u g h o u t t h e s e c t i o n w i t h o u t a p p a r e n t r e l a t i o n t o t h e maf i c m i n e r a l s . T h e s e are presumed t o be t h e p r o d u c t o f hydro the r - m a l a l t e r a t i o n .
f4’ has
Dark brown, p l e o c h r o i c b i o t i t e i s s u b h e d r a l t o e u h e d r a l ,
APPENDIX D
Statement of Costs, Labour, Personnel, etc.
Statement of Expendi tures re R e b e l MAX Claim July - August 1978
a ) Geological Mapping, Sampling, etc.
Sawyer Consultants Inc.
J. B. P. Sawyer , P. Eng. July 12th to 31st , 1978 $1,490. 00 Aug. 1s t to Sept. 5th, 1978 890 .00
T. B. Smart, Geologist July 8th to 31st , 1978 2,070. 00 Aug. l l t h , 14th- l8th, 1978 - 540. 00
$4,990. 00 $4,990.00
A s saying 364.00
141. 51 Draughting and m a p pr int ing, etc.
P e t r ag raphic Studies 277. 50
Off ice , misce l laneous
b ) Line-cutting, P a c k s a c Dril l ing
Labour (J. Sheldon - July 10th to Aug. 8th, 1978) (W. Sheldon - July 10th to Aug. 8th, 1978)
437. 65
2,647. 87
$8,858. 53
Sample Number:
Mineralogy:
RM-3-78 (17 .5)
p l a g i o c l a s e 57 K-fe ldspar 2 2 q u a r t z 1 b i o t i t e 8 w h i t e mica 3 c a r b o n a t e 6 c h l o r i t e 2 z i r c o n , sphene t r opaques 1
C l a s s i f i c a t i o n : modera t e ly a l t e r e d d i o r i t e
F a b r i c and t e x t u r e : medium-grained, e q u i g r a n u l a r , holo- c r y s t a l l i n e , hypid iomorphic-granular
The f a b r i c o f t h i s rock s t r o n g l y resembles RM-1-78 (101). The p r imary c o n s t i t u e n t i s e u h e d r a l t o s u b h e d r a l p l a g i o c l a s e . The l a t h s are randomly o r i e n t e d . A l b i t e and combined carls- b a d - a l b i t e tw inn ing are c h a r a c t e r i s t i c . The p l a g i o c l a s e com- p o s i t i o n i s a n d e s l n e ( A n 4 4 ) , de te rmined by t h e Michel-Levy t e c h n i q u e . Normal zoning i s p r e s e n t . A l t e r a t i o n i s weak t o moderate. Shreds o f w h i t e mica are v i s i b l e a l o n g c l e a v a g e traces and f r a c t u r e s ; calcic cores of zoned g r a i n s are p re - f e r e n t i a l l y a l t e r e d . Carbonate o c c u r s a long t h e p l a g i o c l a s e margins . I t o f t e n a lso a p p e a r s t o be i n t e r s t i t i a l .
K-fe ldspar i s s u b h e d r a l t o a n h e d r a l . I t r a r l y o c c u r s as d i s t i n c t c r y s t a l s , b u t i s t y p i c a l l y i n t e r s t i t i a l t o t h e p l a g i o c l a s e . The K-fe ldspar i s n e i t h e r p e r t h i t i c n o r twinned. Myrmekitic t e x t u r e s are n o t v i s i b l e i n any of t h e f e l d s p a r s . The K- fe ldspa r may be a s s o c i a t e d w i t h a few s h r e d s o f w h i t e m i c a , b u t i t i s g e n e r a l l y u n a l t e r e d . Q u a r t z i n a n h e d r a l , f i l - l i n g t h e i n t e r s t i c i e s among t h e f e l d s p a r s o r o c c u r r i n g as i n - c l u s i o n s i n t h e p l a g i o c l a s e and b i o t i t e .
z i n g a f t e r t h e p l a g i o c l a s e b u t b e f o r e t h e K- fe ldspa r and q u a r t z . I n c l u s i o n s of q u a r t z , a p a t i t e , and opaques are common. Zi rcon i s f r e q u e n t l y a s s o c i a t e d w i t h t h e p l a g i o c l a s e r a t h e r t h a n t h e b i o t i t e . The b i o t i t e i s i n c i p i e n t l y a l t e r e d t o combina t ions of w h i t e mica, c a r b o n a t e , and c h l o r i t e , i n o r d e r o f i n c r e a s i n g abundance. White mica and c h l o r i t e w e r e t h e f i r s t a l t e r a t i o n p r o d u c t s , fo l lowed by c a r b o n a t e . A few s h r e d s of w h i t e mica a re t y p i c a l l y a s s o c i a t e d w i t h masses o f c h l o r i t e ; t h e l a t t e r may r e p l a c e l a r g e p o r t i o n s of i n d i v i d u a l g r a i n s . The c h l o r i t e i s a l s o d isseminated th roughou t t h e s e c t i o n and may i n p a r t r e p l a c e p l a g i o c l a s e . Carbonate is p r e s e n t i n c loudy mosaics r e p l a c i n g b i o t i t c , c h l o r i t e , and a d j a c e n t p l a g i o c l a s e . Anhe- d r a l c l o t s of opaques a r e d i s s e m i n a t e d t h r o u g h o u t , and a re n o t n e c e s s a r i l y r e l a t e d t o b i o t i t e a l t e r a t i o n . These may be e i t h e r magmatic o r hydro thermal i n o r i g i n . Needles of h e m a t i t e ( ? ) are a s s o c i a t e d w i t h t h e b i o t i t e a l t e r a t i o n .
Dark brown, p l e o c h r o i c b i o t i t e i s s u b h e d r a l , c r y s t a l l i -
Sample Number:
Mineralogy:
RM-3-78 (109.9)
groundmass 76 p l a g i o c l a s e 4 muscovi te 1 w h i t e mica 1 0 c a r b o n a t e 9 opaques t r z i r c o n , zeo l i t e t r
C l a s s i f i c a t i o n : a l t e r e d fe l s i te
Fabric and t e x t u r e : h o l o c r y s t a l l i n e , p o r p h y r i t i c i n large p a r t allotriomorphic-granular
Excedingly f i n e - g r a i n e d , f e l s i t i c groundmass p redomina te s i n t h i s s e c t i o n . Q u a r t z o - f e l d s p a t h i c m i n e r a l s o c c u r i n an i n - t e r l o c k i n g mosaic w i t h v e r y i r r e g u l a r g r a i n b o u n d a r i e s . I n d i - v i d u a l g r a i n s cou ld n o t be i d e n t i f i e d i n t h e groundmass. V a r - i a t i o n s i n g r a i n s i z e are v i s i b l e i n hand specim as f a i n t , wavy c o l o u r v a r i a t i o n s . T h i s may r e p r e s e n t t h e c o u n t e r p a r t o f f low banding i n volca-n ic r o c k s .
o c c u r set i n t h e groundmass. Although p e r v a s i v e l y a l t e r e d , remnant t w i n s lamellae o f t h e a l b i t t y p e are v i s i b l e . The p l a - g i o c l a s e compos i t ion , de t e rmined by t h e Michol-Levy t e c h n i q u e r a n g e s from An30 t o An34 ( a n d e s i n e ) . The i n t e r i o r s o f t h e p h e n o c r y s t s are r e p l a c e d by f i n e - g r a i n e d s h r e d of ser ic i te t h a t i m p a r t a g r e e n i s h c o l o u r a t i o n i n hand specimen. The o u t e r margins o f t h e p h e n o c r y s t s are a l t e r e d t o t u r b i d masses o f car- b o n a t e t h a t a p p e a r as l i g h t - c o l o u r e d r i m s i n hand specimen.
l a t h s o f muscovi te . The c l e a v a g e traces of t h e s e p h e n o c r y s t s a re l i n e d w i t h f i n e - g r a i n e d opaques. ‘ I t i s p o s s i b l e t h a t t h e s e muscovi te l a t h s r e p r e s e n t former b i o t i t e l a t h s r e p l a c e d by mus- c o v i t e d u r i n g a l t e r a t i o n .
p l a g i o c l a s e p h e n o c r y s t s i s a l so p r e s e n t i n t h e groundmass. Minute s h r e d s o f w h i t e m i c a are d i s s e m i n a t e d th roughou t t h e groundmass. Turb id mosa ic s of c a r b o n a t e are a l so scattered th roughou t t h e groundmass, b o t h w i t h o u t a p p a r e n t r e l a t i o n t o t h e f e l d s p a r p h e n o c r y s t s . I n several l o c a t i o n , vugs f i l l e d w i t h inward-growing, a c i c u l a r n e e d l e s are associated w i t h t h e c a r b o n a t e . Although i m p o s s i b l e t o i d e n t i f y m i n e r a l o g i c a l l y , t h e s e a c i c u l a r c r y s t a l s may be zeol i tes . C r o s s - c u t t i n g q u a r t z c a r b o n a t e v e i n l e t s are a lso v i s i b l e i n t h e s e c t i o n ; t h e y c u t b o t h t h e groundmass and p h e n o c r y s t s .
Although f i n e r - g r a i n e d and pe rhaps m o r e f e l s i c i n composi- t i o n , t h e f ab r i c of t h i s rock resembles M-15-78 and M-6-78. The rock i s b e l i e v e d t o be a f i n e - g r a i n e d i n t r u s i v e c o u n t e r p a r t o f a d i o r i t e o r a monzoni te ,
Phenoc rys t s o f p l a g i o c l a s e up t o several mm i n d i a m e t e r
Many o f t h e p h e n o c r y s t s are also associated w i t h e u h e d r a l
The w h i t e mica and c a r b o n a t e a l t e r a t i o n which a f f e c t s t h e
Sample Number:
Mineralogy :
RM-4-78 (56')
p l a g i o c l ase 4 1 K-fe ldspar 18 q u a r t z 6 c a r b o n a t e 18
w h i t e m i c a 1 4 a p a t i t e , z i r c o n t r sphene , zeol i te t r
opaques 2
c l a s s i f i c a t i o n : a l tered d i o r i t e
F a b r i c and t e x t u r e : The o r i g i n a l rock f a b r i c i s v e r y s i m i - l a r t o RM-1-78 ( 1 3 1 ' ) ; however, a l t e r a t i o n masks t h e o r i g i n a l t e x t u r e . I t w a s presumably medium-grained, e q u i g r a n u l a r , ho- l o c r y s t a l l i n e , and hypid iomorphic g r a n u l a r . Euhedra l t o sub- h e d r a l p l a g i o c l a s e l a t h s show b o t h a l b i t e and combined carls- b a d - a l b i t e twinning . The Michel-Levy t e c h n i q u e w a s u sed t o d e t e r m i n e t h e p l a g i o c l a s e composi t ion ( a n d e s i n e , An37) . The p l a g i o c l a s e h a s been p e r v a s i v e l y al tered d u r i n g t w o s e p a r a t e a l t e r a t i o n e v e n t s . The ear l ie r a l t e r a t i o n c o n s i s t s of n e a r l y complete r ep lacemen t by w h i t e mica /c l ays . O r i g i n a l o u t l i n e s o f p l a g i o c l a s e l a t h s are v i s i b l e , b u t tw in lamellae are pre- s e n t o n l y i n o c c a s i o n a l g r a i n s . The second a l t e r a t i o n e v e n t c o n s i s t s o f n e a r l y complete o v e r p r i n t i n g by c a r b o n a t e . The o r i g i n a l morphology o f t h e g r a i n s is s t i l l v i s i b l e , b u t any remain ing f e l d s p a r , as w e l l as some of t h e w h i t e m i c a , i s re- p l a c e d by c a r b o n a t e .
I ( - fe ldspar and q u a r t z are s u b h e d r a l and a n h e d r a l , r e spec - t i v e l y . The o c c u r i n t e r s t i t i a l l y among t h e p l a g i o c l a s e l a t h s , and q u a r t z i s i n t e r s t i t l a 1 t o b o t h f e l d s p a r s . The w h i t e mica a l t e r a t i o n h a s n o t s i g n i f i c a n t l y a f f e c t e d t h e K- fe ldspa r ; how- e v e r , even t h e R- fe ldspa r i s r e p l a c e d by c a r b o n a t e . Only t h e q u a r t z remains u n a l t e r e d by t h e second s tage a l t e r a t i o n . V a r - i a t i o n s i n t h e i n t e n s i t y o f a l t e r a t i o n are v i s i b l e i n hand specimen a s d i f f e r e n c e s i n c o l o u r .
Euhedra l t o s u b h e d r a l b i o t i t e has been comple t e ly re- p l a c e d by w h i t e m i c a and c a r b o n a t e . The r e p l a c e d b i o t i t e i s a s s o c i a t e d w i t h a p a t i t e , z i r c o n , sphene , opaques , and occa- s i o n a l muscovi te . The muscovi te may be t h e ear l ies t a l t e r - a t i o n , p a r t i a l l y u n a f f e c t e d by t h e c a r b o n a t e . The o r i g i n a l morphology of t h e b i o t i t e i s marked by t r a i n s of opaques a l o n g t h e c l e a v a g e t r a c e s . The o r i g i n a l b i o t i t e w a s a s s o c i a t e d w i t h r e l a t i v e l y h igh p r o p o r t i o n s of sphene , which remains u n a f f e c - t e d by t h e i n t e n s e a l t e r a t i o n . A c i c u l a r growths o f z e o l i t e ( ? ) are a s s o c i a t e d a s i n F3l-1-78 ( 1 0 1 ' ) . M i c r o v e i n l e t s o f q u a r t z c r o s s - c u t t he s e c t i o n and are u n a l t e r e d , a l t h o u g h ear l ie r t h a n t h e c a r b o n a t e .
The es t imated f e l d s p a r r a t i o and p l a g i o c l a s e composi t ion s u g g e s t t h a t t h e o r i q i n a l rock w a s a d i o r i t e . The a l t e r a t i o n i s presumed t o be of hydro thermal o r i g i n ; i t c o r r e s p o n d s t o " p r o p y l i t i c " a l t e r a t i o n of Lowell and G u i l b e r t .
f ! ‘I
P e r s o n n e l and Da tes re W o r k ‘,n R e b e l Developments Ltd. MAX CLAIM - Ju ly and A u g u s t , 1 9 7 8 -- - ---_-_I_
R e b e l Developmvnts Ltd. --
J. Sheldon
W. Sheldon
Ju ly 10th t o A u g u s t 8 t h ,
Ju ly 10th ti) A l l g u s t 8 th .
1978
1978
Sawyer Cqnsul tan ts Inc.
J. B. P. S a w y e r , P. Eng.
( F i e l d ) July 12 th tc, I b t h , 1978 inc lus ive
(Off ice) ATigus t 9ch a n d lo th , 1978
T. B. Smart , Geologis t
( F i e l d ) July 9th tc, 31s t , 1978 inc lus ive
(0 ff i c e ) A u g u s t I I t h , 14tE,-18th, 1978 inc lus ive
Rebel Developmentr Ltd., 3 - 425 Howe Street, Vancouver, B.C. V6C 2A9
July 3 1 s t , 1978
,
in account with Sawyer Consultants Inc. i
1
To Profesmional Servicor. ,
I Re Max Claim Work. . I
July 12-16 inclusive - 5 field day6 @ $200.00 I I
i $1,000.00 f/
July 5,6,10,21,25,27-31 - 14 hours @ $35.00 490.00
Disbursementrt
J. B. P. Sawyer expenme#, a s per attached $ 350.21
T. B. Snurk. goologirt - 23 d8ys @ $90.00 2,070. 00 i/
b
I B.C. Telephone Co. - July 24/78 billing 24.61
Vancouver Petrogrrphics - Mark Bloom
Bondar-Clegg & Co. Ltd. - geochem bagr
report, invoice #1348
invoice 11998
227. 50 /
44.10 i/
P. W.A. - air cargo
Superior Reproductionr Ud. - invoice #R6533 1
Mire J. F.rQuh8r6On - typing and office
15.00 V'
7.41 V'
44.00 L/
11.10
2.85
50
ar r i s tance - account July 3 1 /78
In-office copying - 74 Q $IS$
Mining Recorder - map, invoice d158654G
CBA - parcel delivery, invoice 1814504 9. 00
Canada Por t - July 2 1/78
Total Dieburremants $2,806.28 2,806.20
I
i
TOTAL INVOICE . $4,296.28 - : * :
INVOICE Nr 1348
_- OUANTllY DESCRIPTION
THtN SECnONS $ 4 . 0 0 ~
POLISHED THIN SECTIONS
POLISHED ORE MOUNTS
GROUND LABELLED THIN SECTWON REJECT SLICES
POLISHED MINERAL GRAIN MOUNTS
MINERAL GRAIN THIN SECTIONS MINERAL GRAIN POLISHED THIN SECTIONS
THIN SECTION KSPAR STAINS
ROCK KSPAR STAINS
CERAMIC NJLVERIZER PLATES U P P E D
--
- --
PETROGRAPHIC REPORT by m k S, Bloom
FED. TAX
mov. TAX -
SHl PQl NG
TOTAL (Canadian Funds 1
Customer Order No.
Customer Charge Code
-1
$227.50
* i . Ordered By FOR
i ~ - - ~
.
8 1998 INVGICE. 8 1 9 9 8
Savyer Consultento La.
vancomr, bC. VY: 2A9 11 - 42s a- 8e-t
DATE. J u l y 25, 1978
REPORT NO. t i
PROJECT:
@ $ 37.50/M $ 37.50
+ 12% FST 4.50
$ 42.00
+ 5% PST 2.10
. . 1
t
...
J*lL 7
m/
0
T - I
---t t... +-
-... . .
!
August l l th , 1978
Rebel Developmento Ltd. , 3 - 425 Howe Street, Vancouver, B.C. V6G 2A9
in account with Sswyor Consultanto Inc.
To Professional Setvicer.
Auguet lot-7th, 1978 - field and travel, 7 days @ $90.00 $ 630.00 r /
Estimate 4 days office re plotting data, etc. @ $90.00 as instructed by A. Areenault
360.00 1/
J.B.P. Sawyer
Diebursementst
Bondar-Clegg & Go. - assaying Plue Collect ehipping charge
Total Dirbursernent I
Less Bal8nce on hand from advance
300.00 J
$ 1 , 2 9 0 . 0 0
$342. OOw' 13.00
$355.00 355.00 J
Note: Additional Disbursements to be invoiced later include typing and office asristance, draughting, and long distance telephone calls.
$1,645.00
703.72
$941.28
October 28th, 1978
Rebel Dovolopmantr Ud., 3 - 425 Haw. Stroot, Voncouvor, B.C. V6C M 9
in account with S.wyer Conrultantr Inc.
To P r o f o r a i o ~ l Servicar.
J. B. P. Sawyer, P. Eng.
Re Proparation of Roport on brr Claim work July 1978. Revirion of Report and addition of personnel stc. record8 for Arrorrmont filing.
2 dayr @ $200.0O/day
Ro Proprratiaa of B. C. Dept. Miner forms ro reduction of tlaimr, Noticor to Group, 8nd Strtoment of Explorrtion C Devolopmont, and of accounting back-up documentation.
Corrospondenco, phono calla, maetingr, etc. re A r r enau1t Claim di r put..
Contrctr with H. Wober, Chovron Minsrdr , L. D'Aigls, Canada Twgrton re Arreaault chimr and tranrmittal of report to Wober, otc.
Aug. 11, 17, 18, 21; Sept. 6 , 7, 11, 15, 27; Oct. 28, 1978.
14 hourr @ $35.OO/hr.
Sub Tot81 Less, invoiced Aug. 11 / 78
Balance
Dirburromentr a0 por attached 1i.t
TOTAL f O I C E
$ 400.00 L//
490.00
$ 890.00 300.00
$ 590.00
1,088.99 L/'
$1,678.90
- Notet Long dirtanco c h r g o r to be invoiced later. I
j D ir burremontr I I I T. B. SmrL - office re Max Claim mrpr, etc.
Lees invoiced Aug. 11/78 360.00
Balance duo $180.00 $ 180.00 /
Aug. 1 1 , 14-18 inel., 6 dry0 @ $90.00 $540.00 ~
I
T. B. Smart - oxpenre account dated Aty. 21/78 55.37
C. L. Cory - draughting Account Sept. 18/78 Account oc t . 5/78
Bondar-Clegg & co. - 8rsaying Invoice B2481, Aug. 17/78
Superior Roproductionr - map printing m d photocopying lava ic e I #R67 3 89
UR030351 1YR73175
B.C. Te1 - long dietancs charger Account Aug. 24/78
Sept. 23/78
B. C. Hydro t Power , Aug. 28/78
In-office copying - 179 @ l5$
J. Farquharron - office aerirtance, Aug. 18 to Oct. 28/78
$320.00 I/
$340.00 340.00
20.00 J
$34.85 d' 6 . 3 5 I/'
54.95
$96.15
$10.80 13. S l -
$24.31
9.00
96.1) v/
24.31
8.06
26.85 i/.
349.25 1/
$1,088.99
rl , . - - .~ . . .. +' - ;oivirAi.u'Y - . ~. .~. L I u.
7&4 BELFAST ROAD, OTTAWA, ONTARIO. K9G O T C L ' t4 [~ l>JE. 237 - 3 1 1 0 TELEX. 053-3548
Sawyer Consultants Inc. A 1 - 425 Howe Street Vancouver, B. C . V6C 7A9
1 Tungsten
SaWYER CONSCILTANTS INC 1-425 HOWE STREET VQNCOCIWR BC
REBEL
K x
F.S.T. NO.
OUOTE BY
BILL Bv:
PROV TAX NO
OUOTE PRICE
BILL DATE ? 1 /OF: ,'-78
TERMS N E T 30 DAYS
TAXABLE
FST
SWTOTAL
PROV. TAX SUBTOTAL
REMITTO: SUPERIOR REPRODUCTIONS LTD. W M m L v u c LT.. VANCOUVER e c VIE 1.1
A S f R V l C E L O U n O N S 1111 MELVILLE Sl, 435 HOWE ST - LOWER BEWTALL Il l * 2407 BURRlRD ST. bT&-
SAWYER C:nNSlJLTCINTS TNC 1-425 HOWE !?TREET VCINCDI IL'ER RC
us13 2AO
4160 Pr ince Albert S t r ee t Vancouver, 13. C. V5V 4J4 October 28, 1978
Sawyer Consultants Inc., 1 - 425 Howe St ree t , Vancouver, B.C. V6C 2A9
in account with J. Farquha r son
To office se rv i ces re Rebel Developments Ltd. Aug. 18 to Oct. 28, 1978.
63 1 / 2 hours @ $5.50 =
Received Payment ,,
m I.
-. . ._ .__ . . .- I - - . - . _I__.._.______._
I------- - /
OF 5 P A G t 1 Diamond Drill Kecord COMPANY NAME -Rebel Developments Ltd, HOLE NO EM-1
CLAIM NAMf/No. M PROPERTY NAME M ~ - - _ _ - . - ___ - - - _- .
DRlLLlNG CONTRACTOR COMMENCED 2 3 / 7 / 7 8 ~
LOGGED BY
_ _ _
e pink garnet , porphyritic texture.
e sulphide specks. ______-
__ _____ ___.____ ____ . _ - 9 grey in colour; _ _ _ __ __ - __--_
with minute white c rys ta l s of sulphide. _ _ _ ~ ~ ____ -
__ .
--______- - with impregnations of a dark minera l to _-__. give speckled
.-
COLLAR: HOLE SURVEY FOOTAGE AZIMUTH DIP _-
-__. .-
ELEVATION _ _
LOGGED BY ~- _-__ - -
Diamond Drill Kecord COMPANY NAME - .___________ - ..___ ________ PROPERTY NAME _ _ _ _ ____ - - - - _ . __ - - - __
DRlLLlNG CONTRACTOR - ____ ASSAY E R
1 I PURPOSE OF HOLE __ _____ __ __ - - ~ _ _ DATE LOGGED MAP REFERENCE NO METHOD
HOLE NO _____-._ EM- 1 CLAIM NAME/No.---
COMMENCCD
F I N ISHE D
PROJECT NO
J
SAMPLE ASSAYS - FROM 7 0 WIDTH NO
FROM TO RECOVY DESCR l PTl ON
0 * 18.0-20 .0 - q u a r t z bands with c o r e angle 45 -~ - - a l s o along c o r e -
r y s i l iceous, m i n o r sporadic sulphide ___ specks.
to c o r e axis. _ ~ _ __________ ~
__ - - _- - . ___ - - -
ith occasional specks of pyri te . _ _ _________
___. .
d a r k __-- brown, pink - - g a r n e t . __ and E o b a b l e chiastol i te as a
m e d c r y s t a l and d a r k cent re . ____ .____ __ ___ - ___
o d a r k brown w i t h g r e e n i s h ___ a n d p _______
. 0-52. 0 ) , d a r k br,own, biotite. -__ -
---1- HOLE SURVEY Diamond Drill Kecord PAGE 3 OF COLLAR.
I I COMPANY NAME - _______- HOLE NO EM-1 FOOTAGE I AZIMUTH I DIP 1 CLAIM NAME/NO. -
COMMENCED
F I N ISHE D
PROJECT N O
PROPERTY NAME
DRlLLlNG CONTRACTOR ~ - _
ASSAY E R
ELEVATION
LOGGED BY -
DATE LOGGED PURPOSE OF HOLE MAP REFERENCE NO METHOD.
____ *
SAMPLE ASSAYS
FROM T O WIDTH NO FROM TO RECOVY DESC R 1 PTl ON
0 0 I r regular banding wi th darker ma te r i a l (core axis -
45 -75 ). _- I
-__ ~
ose wi th minor
__ __ ___ _ _
COLLAR HOLE SURVEY Uiarnond l)ri&A Kecord tAbt 4 OF L -
FOOTAGE AZIMUTH DIP HOLE NO EM-1 COMPANY NAME - - -
PROPERTY NAME _____--- __ __ CLAIM NAME/&. ELEVATION
LOGGED BY ___--_- DATE LOGGED MAP REFERENCE NO METHOD
DRI LLlNG CONTRACTOR COMMENCED
ASSAY E R PURPOSE OF HOLE - PROJECT NO
F I N ISHED
$
ASSAYS SAMPLE FROM TO WIDTH NO
FROM TO RECOVY DESC R 1 PTl ON
102-103 - approximately 6" quartz vein with sphalerite and l a rge
pyri te 1 /4" crys ta l s .
103. 0-105. 0 - fine s t r inge r s containing white sulphide and rock
with fine disseminated white sulphide.
105. 0-1 10. 0 - quartzi t ic hornfels.
Py r i t e blebs 112.0- 113.0, occasional.
116. 0-118.0 - dark and l ighter banded hornfels ic rock.
minor 1 /2" white quartz vein with pyri te , and minor amounts of
s p ha le r it e . 118. 0-1 19. 0 - hornfels with sma l l amount of white quartz.
_____.
- - ____ __ - 0
- Core ax is 55 a t 110. 0. ____ ____ __
____ _ _ _
At 117. 5 _____ -
~
- _ _ _ _ _ _ ~ _ _ _ _ _ _ _ _ _ _ _ _ - - - _ _ - __ - --
- _____ _____ __ - _____ _ _ - - -- ____--- - -
119. -___ 0-120. 0 - s o m 9 y r i t e _ _ __ - in -~ blebs and lenses. - .. -
1 I
I
ELEVATION
LOGGED BY
r HOLE NO
CLAIM NAME/No.
COMMENCED
FINISHED
PROJECT NO DATE LOGGED MAP REFERENCE NO.
Diamond Drill Kecord COMPANY NAME - PROPERTY NAME
DR I LLlNG CONTRACTOR ASSAY E R
PURPOSE OF HOLE
________- __
I 1 METHOD:
1 SAMPLE ASSAYS
FROM TO WIDTH NO FROM TO RECOVY DESC R I PT I ON
Garnetiferous. ? sulphide.
127 132 5' ish colour in __
132 137 5'
ite as fine s t r ia ted white
ansparent mine ra l 137 142 5'
-__I_ ore noticeable on -
142 147 5 ' ______
spots. ___
- 147 152 5 '
- -
152.0 170.C Hornfels : Dark brown in colour, var iable siliceous.
152.0-153.0 - pyrit ic bands and blebs.
- .-- -- --- - 154. 0-159. 0 - fine s t r ingers of white sulphide. - ___ --
159. 0-161. 0 - occasional pyrite blebs.
161. 0-170. 0 - blebs of white sulphide a t intervals; f r ac tu re planes
-
