by: graham bubner chris gaughanchris gaughan paul...
TRANSCRIPT
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The Iron Magnet DepositBBy:Graham BubnerChris GaughanChris GaughanPaul Leevers
Mines Presentation - Jan 2004
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INTRODUCTION
• LOCATION
• BRIEF HISTORY OF THE DEVELOPMENT OF THE IRON MAGNET DEPOSITTHE IRON MAGNET DEPOSIT
• GENERAL GEOLOGY OF IRON MAGNET
• MINERALISATION CONTROLS AND STYLES
• GEOPHYSICAL SIGNATURES
Mines Presentation - Jan 2004
• CURRENT WORK
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LOCATION
Port Augusta
WHYALLAIron Knob
Iron BaronIron Duke
IRON KNOB(CLOSED)
N
South Australia
ADELAIDE
Kangaroo Island
Ardrossan
Coffin Bay
Cooyerdoo
Katunga Hills
QUARTZ QUARRY
South Australia
IRON BARONCamel Hills
North Middleback
Range
(CLOSED)
WHYALLARange
IRON KNIGHT
IRON DUCHESS South MiddlebackRange
Mines Presentation - Jan 2004
IRON DUKESpencer Gulf
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Mines Presentation - Jan 2004
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Mines Presentation - Jan 2004
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HISTORY
• EARLY 1960’S - SIGNIFICANT MAGNETITE MINERALISATION INTERCEPTED AT IRON DUKE AND IRON DUCHESS
• 1967 - AN ADIT WAS DEVELOPED AT NORTH END OF IRON DUKE AND ENCOUNTERED SIGNIFICANT MAGNETITE MINERALISATIONMAGNETITE MINERALISATION
• 1989 – FIRST SERIOUS ATTEMPT TO ESTABLISH A MAGNETITE RESOURCE ~ 33 DDH, 7400M CORE, 2.5 KM STRIKE LENGTH
EARLY 2002 A REVIEW OF THE DOWNSTREAM• EARLY 2002 – A REVIEW OF THE DOWNSTREAM PROCESSING BENEFITS OF USING MAGNETITE AS FEED TO THE WHYALLA STEELWORKS LEADS TO THE CURRENT WORK BEING UNDERTAKEN
Mines Presentation - Jan 2004
CURRENT WORK BEING UNDERTAKEN
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REGIONAL SETTING
Mines Presentation - Jan 2004
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TRADITIONAL MIDDLEBACK SUBGROUP STRATIGRAGHYTRADITIONAL MIDDLEBACK SUBGROUP STRATIGRAGHY
Oxide Facies
Silicate Facies
THIC
K Upper Middleback Jaspilite
CarbonateFacies
500
m
T
Cook Gap Schist
OxideFaciesPR
OX.
2 Cook Gap Schist
Facies
SilicateFacies
Carbonate
APP
Lower Middleback JaspiliteFacies
Sulfide UnitKatunga DolomiteBasal SchistE
Mines Presentation - Jan 2004
1000
m TH
ICK Basal Schist
Warrow Quartzite
IRO
N O
RE
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MINE SEQUENCE STRATIGRAPHYCook Gap Schist
Sheared contact
Jaspilite
Magnetite silica MTS
JAS
Magnetite talc
Talc schist and other various talc, magnetite, chlorite & quartz schists
(Lower)Middleback
Iron Formation
MTT
MTSMTT
Hematite-magnetitecarbonate
Magnetite carbonateIron Formation
HMO
MTC
MTCHematite Ore
Basal Seq ence
Hematite Carbonate
BSQ
HEO
HEC
MTC
HEO
BSQ BSQ
Sulphide unit
Basal Sequence
Katunga Dolomitewith intercalated volcanics
BSQ
++++ ++
SBX
DOM
Mines Presentation - Jan 2004
Sleaford Complex ++ ++++++++++ ++ ++
++ ++++++
++++
++++ ++
++++++
++++ ++Lincoln Complex
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1500
Regional Deformation HistoryRegional Deformation History
AK
AN
EV
ENT 1500
Broad Cross Folding on E - W AxisNW - SE FaultingD4
WA
TA
East - West Compression.
1540
1710p
Broad Regional Folding, Variable PlungesUpper Green Schist FaciesP - T 1.5 - 2 Kb 450 - 525 o C
1745
D3
Major Mylonite Development
East - West CompressionTight Isoclinal FoldingA
N
OR
OG
ENY 1745
D2g g
Upper Amphibolite FaciesP - t 5 - 7 Kb 600 - 675 o C
KIM
BA
1795
Mines Presentation - Jan 2004
Early Layer Parallel Schistosity
1845
D1
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STRUCTURAL INFLUENCED2 - D2 folding is the major influence on the geometry and
distribution of mineralised host lithologies. The main controlling feature appears to be a large scale parasiticcontrolling feature appears to be a large scale parasitic syncline-anticline pair, which occurs on the west-limb of a much larger syncline.• Thickening in fold hinges is indicated at outcrop scale• Thickening in fold hinges is indicated at outcrop scale
• D3 -Main influence of D3 is the development of regional myolinite and local shear zones which bound the deposit on both sidesboth sides.
• D4 – NNW NW NE AND NNE faults are present
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Section @ 16575N
Mines Presentation - Jan 2004
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MINERALISATION STYLES• Selective replacement of layers at all scales from
laminae to beds
• Pervasive replacement of layers at all scales from laminae to beds
• Matrix to breccias and clasts within breccias
• Open space filling in fractured carbonate, bedding-parting and any other odd cracks and openings
Di i t d d tt i li ti• Disseminated and spotty mineralisation
• Poorly developed stockwork veining
Mines Presentation - Jan 2004
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MINERALISATION• STRATABOUND – MTC-MTS W/MTT AT BOUNDARYS OUN C S W/ OUN
• WITH HIGH GRADE POLYMICT MATRIX SUPPORTED BRECCIAS – MATRIX OF MASSIVE MAGNETITE
•MULTIPLE STYLES
•SPATIAL ASSOCIATION W/ AMPHIBOLITE DYKES ON EASTERN SIDE OF DEPOSITEASTERN SIDE OF DEPOSIT
•FEEDER ZONES?
INTERPRETATION
• HYDROTHERMAL-METASOMATIC SEDIMENTARY CARBONATE REPLACEMENT DEPOSIT
•IN ASSOCIATION WITH GRANITIC INTRUSION?
•IN ASSOCIATION WITH METAMORPHISM?
SKARN STYLE OF MINERALISATION?
Mines Presentation - Jan 2004
•SKARN STYLE OF MINERALISATION?
•LITHOLOGICAL FACIES CONTROL ON MINERALISATION
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BRECCIA AND CARBONATE VEIN
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Massive Magnetite in MTC
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Breccia with Massive Magnetite
Mines Presentation - Jan 2004
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GRADE DISTRIBUTION
%SiO2 MASS REC MAG FE%SiO2 MASS REC
Target Concentrate – 69.5% Fe, 1.8% SiO2
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Magnetite Magnetite Resources and ReservesResources and Reserves
Resources
Iron Magnet – 234 Mt at >37% IronIron Magnet 234 Mt at 37% Iron
Reserves
Iron Magnet 72 2Mt @ >43% Iron Iron Magnet – 72.2Mt @ >43% Iron
Mines Presentation - Jan 2004
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Project Magnet – In Fill Drilling
Mines Presentation - Jan 2004
Phase 3 Drill Out Programme 26,000m RC
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GEOPHYSICS AT IRON MAGNET CONTROLLED GEOPHYSICAL DATA CAN BE
USED TO ACCURATELY MEASURE MAGNETITE DISTRIBUTION AND CONTENT AT
DEPOSIT SCALE DRILLHOLE SCALE BLASTHOLE SCALE BLASTHOLE SCALE
INTERPRETED RESOURCE FIGURE FROM GROUND MAGNETICS
Mines Presentation - Jan 2004
CALCULATION OF MAGNETITE CONTENT FROM DOWNHOLE & CORE PETROPHYSICS
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DETAILED GRAVITY & GROUND MAGNETICS WERE ACQUIRED OVER THE MIDDLEBACK RANGES IN 1997
PROFILES OF GROUNDPROFILES OF GROUND MAGNETIC INTENSITY ON
10 x 150 METRE GRID
MAX. ANOMALY ~ 25,000 nTMAX. ANOMALY 25,000 nT
Mines Presentation - Jan 2004 400 METRES
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INTERPRETATION ON 100m SECTIONS INCLUDED ALL AVAILABLE ASSAY DATA FROM HISTORICAL DRILLING
OBSERVED GRAVITY IRON MAGNETOBSERVED GRAVITY
CALCULATED GRAVITY9
mG
al
IRON MAGNET
SECTION 6316400N
OBSERVED MAGNETICS
CALCULATED MAGNETICS00
0 n
T
CALCULATED MAGNETICS
10
,0e
tre
s
SCH
HEMATITE ORE
AMPH
50
0 M
e
COOKS
“BASEMENT” HMO
MHO
INTERPRETED MAGNETITE
Mines Presentation - Jan 2004
COOKS
RANGEUNDIFFERENTIATED
MIDDLEBACKS
ORE SHOWN IN PURPLE
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DRILLHOLE RESULTS CONSISTENT WITH GEOPHYSICAL INTERPRETATION (VERY FEW ‘WASTED’ DRILLHOLES)
15 000 METRES OF DRILLING15,000 METRES OF DRILLING
HEMATITE
ORE
AMPH
SCHHMO
MHO
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INITIAL PRE-DRILLING GEOPHYSICAL MODEL SUGGESTED A RESOURCE OF 71 Mt > 40% mtt
North
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CALCULATION OF WEIGHT % MAGNETITE FROM DOWNHOLE & CORE GEOPHYSICS
IRON MAGNETSIX REPEAT LOGS
ALL DOWNHOLE & CORE MEASUREMENTS OF DENSITY & MAG SUSC SUBJECT TO
DD03IM009CALIBRATIONS
19-AUG-200303-NOV-200310-JAN-200417-JAN-200424-FEB-200405-MAR-04
SIX REPEAT LOGS OF CALIBRATION HOLE 150-200m
MAG SUSC (SI)
& MAG SUSC. SUBJECT TO QUALITY CONTROL 150
155
0.0 0.5 1.0 1.5 2.0 2.5
MAGNETIC SUSCEPTIBILITY (SI)0 2.5
DEFINED PROCEDURES DUPLICATES (i.e. REPEAT
READINGS) STANDARDS (i CALIBRATION
160
165
STANDARDS (i.e. CALIBRATION HOLES & STANDARDS)
ALL DOWNHOLE LOGGING COMPLETED WITH SAME VEHICLE
170
175
180COMPLETED WITH SAME VEHICLE & PROBES
ALL QC DATA VERIFIED, DOCUMENTED & STORED IN
80
185
190
Mines Presentation - Jan 2004
READILY RETRIEVABLE FORMAT TO SATISFY AUDIT TRAIL
195
200
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PETROPHYSICS DATA FROM FIRST 20 DRILLHOLES PLOTTED AGAINST DTR MAGNETITE CONTENT TO ESTABLISH CORRELATION EQUATIONS
CORRELATION USING DOWNHOLE DATA IN RC HOLESCONTROLLED & FILTERED DATA
70 n = 227TY
50
60
n = 227R2 = 0.910
y = 4.8x2 + 31.2x
R &
DE
NS
IT
40
50
ME
% M
ttE
FR
OM
DT
R
20
30
VOLU
MA
GN
ET
ITE
0
10
VO
LUM
E %
Mines Presentation - Jan 2004
0.0 0.5 1.0 1.5 2.0 2.5SUSCEPTIBILITY (SI)SUSCEPTIBILITY PROBE RESPONSE (SI)
V
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SUMMARY GRAPH OF ALL PARAMETERS RELEVANT TO CALCULATION OF MAGNETITE CONTENT
RELATIONSHIP BETWEEN DEVICE RESPONSE, TRUE SUSCEPTIBILITY AND PERCENT MAGNETITE FOR IRON MAGNET LITHOLOGIES
4.0 100Device response in this region
3.2
3.6I)
80
90
E
Device response in this region >2.5 SI - Uncontrolled data
2.0
2.4
2.8
SPO
NSE
(S
50
60
70
MA
GN
ETIT
E
1.2
1.6
2.0
DEV
ICE
RES
30
40
50
PER
CEN
T
Susc Probe in NQ hole Susc Probe in RC hole
GMS2 t C
0 0
0.4
0.8
0
10
20 GMS2 meter on Core
Volume % Magnetite Weight % Magnetite
Mines Presentation - Jan 2004
0.00 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16
TRUE SUSCEPTIBILITY (SI)
0
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CALCULATION OF WEIGHT % MAGNETITE CALCULATED FROM DOWNHOLE & CORE PETROPHYSICS COMPARED WITH DTR
GRAPH SHOWS, FROMLEFT TO RIGHT :1. CALIPER.2 DENSITY
ONESTEELIRON MAGNET
DD03IM001
0 4 8 12 16 20
CALIPER Cm
ONESTEELIRON MAGNET
DD03IM001
0 1 2 3 4 5
DENSITY GM/ccDENSITY VALIDATEDAGAINST CALIPER
CORE DENSITY
ONESTEELIRON MAGNET
DD03IM001
0 0 0 5 1 0 1 5 2 0 2 5
SUSCEPTIBILITY SISUSCEPT.(CORE) SI
ONESTEELIRON MAGNET
DD03IM001CALCULATED WT % Mtt FROM DOWNHOLE DATACALCULATED WT % Mtt
FROM CORE DATA
0 20 40 60 80 100
DTR MASS RECOVERY %
2. DENSITY.3. SUSCEPTIBILITY.4. WEIGHT % MAGNETITE.
0
20
40
0 4 8 12 16 20 0 1 2 3 4 5 0.0 0.5 1.0 1.5 2.0 2.50
20
40
0 20 40 60 80 100
DATA IN UPPER PARTOF HOLE FROM DOWNHOLELOGGING.
60
80
60
80
DATA IN LOWER PARTOF HOLE FROM COREMEASUREMENTS.
100
120
100
120
CALCULATED % Mtt FROMGEOPHYSICS (RED) SHOWS
140
160
180
140
160
180
Mines Presentation - Jan 2004
GEOPHYSICS (RED) SHOWSEXCELLENT CORRELATIONWITH DTR (BLUE).
200
220
200
220
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WHAT DOES IT ALL MEAN ? FINE-TUNING GEOPHYSICAL MODEL POST-DRILLING
SUGGESTS RESOURCE OF 70 Mt > 40% MAGNETITE, COMPARED WITH JORC INFERRED STATUS OF 64 MtCOMPARED WITH JORC INFERRED STATUS OF 64 Mt.
ANY SUSCEPTIBILITY MEASUREMENT ON ANY SAMPLE TYPE CAN BE QUICKLY & ACCURATELYSAMPLE TYPE CAN BE QUICKLY & ACCURATELY CONVERTED TO A VOLUME (OR WEIGHT) PERCENT MAGNETITE.
SIGNIFICANT SAVINGS TO DATE THROUGH OPTIMISING DRILLHOLE TARGETING.
TECHNOLOGY & PROCEDURES CAN BE ADAPTED TO BLASTHOLE LOGGING TO AUGMENT GRADE CONTROL – SUBSTANTIAL SAVINGS OVER LIFE-OF-MINE OPERATIONS
Mines Presentation - Jan 2004
MINE OPERATIONS.
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GEOPHYSICS AT IRON MAGNET
ADDING VALUE
WITH ZEROWITH ZERO SAFETY,
ENVIRONMENTAL OR CULTURALOR CULTURAL
INCIDENTS, INCURSIONS OR
BREACHES
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Mines Presentation - Jan 2004
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Bedded MTT / MTO
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Magnetite silica
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Transgressive Replacement
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Mines Presentation - Jan 2004
![Page 37: By: Graham Bubner Chris GaughanChris Gaughan Paul Leeverssaemc.com.au/archive/2004/04onesteel.pdf · • brief history of the development of ... of hole from downhole logging. 60](https://reader034.vdocuments.mx/reader034/viewer/2022052005/6018f1d32d72b60f0a572240/html5/thumbnails/37.jpg)
Sheared Magnetite Carbonate
Mines Presentation - Jan 2004