-
28,1102,9
-17,6
56,04,5
49,2
32,6
60,0
5,4
12,4517,0
24,0
38,5
WL
WL
135,0-75,0
13,815,8
9,84,5
13,215,2
13,6
12,0
19,5
22,5
23,8
16,3
47,5
34,5
1,188,5
8,083,89,9
75,072,0
50,9
65,0
48,045,3
53,0
-2,0 72,0
36,0
75,0
38,0
24,737,1 120,7125,6 34,4
127,6 27,4
F1
30,0
F2L3
L2
F3,4,5
L2
F3,4
L1
F5
F1
F2L2
L1
L5
L3
F5
L4F3
F4
L2L2
L1F1
L5
F2F3,4
F5
86,6 86,0
Krivodol formation - krN1S
Uplift "Gangiova - Dabuleni"
Berbesti formation - N2d1
Arc
har f
orm
atio
n -
arN 1
P2
Smirn
ensk
i form
ation
- smN
1m-
P1
Cartajani formation - N
1 P
L1
L'1
L'1
B6/
160,
00
B8/
145,
40
B4/
112,
62B5/
124,
32
B21
/89,
58
B38
4/93
,70/
1967
.
B12
/93,
93/2
008
.
B5/
42,5
0/20
11
.
/27,
03/1
961
.
S4/2
9,45
1/60
,00
2IN
H/5
6,30
6014
2/11
5,46 INH
/131
,04eo
l-elQ
P2-3
elQ
h
eol-e
lQP3
alQ
P2-3
alQ
P2
alQ
h
alQ
P2
alQ
P1
Dan
ube
rive
r/25
,00
0,94 Ma
Tcib
ritc
ari
ver
0,80 Ma
-59,4
-18,2
2,59 Ma30,8
0,80 Ma113,9 17,1
-85,6
505,0
11,5
41,4
8,5
50,0
43,7
25,098,3
30,0
B13
/114
,00
Bru
sarc
i for
mat
ion
-brN
2d-r
Floren
tina
forma
tion -
flN 1
S
Jiu - Motru formation - N2d-r
C1/
26,7
6/19
61
.
/35,
80/1
967
. 47B
C/6
4,45
B4/
70,0
eol-e
lQP2
-3
eol-e
lQP2
-3
alQ
P2
eol-e
lQP2
-3
B7/
155,
00
elQ
h
alQP1
2,59 Ma
0,94 Ma
OEAL S T7 S T6 T2 T1 T0 T0 S T6 OEALS T7
160,0 m
140,0
120,0
100,0
80,0
60,0
40,0
20,0
0,0
-20,0
-40,0
-60,0
-80,0
WL
150,0
174,8
Legend:
Humus clay, contemporary soil (C)
0
Loess, microporous, yellow, Aeolian (L)
Loess-like clay, brown-red, fossil soil (F)
Sandy clay, alluvium
Gravel and gravelly sand, alluvium
Sand, medium-grained, alluvium
Silty clay, variegated to grey, with coal intercalations(Brusarci and Jiu - Motru formations)
Erosion surface
Lithological boundary
Discharge of the aquifer layer from the Archar and Berbesti formationsin the alluvium of the Danube River
Alluvium, Lower Pleistocene - OEAL
Sand, fine- to medium-grained(Brusarci and Jiu - Motru formations)Clayey sand, fine, water saturated(Archar and Berbesti formations)Clay, slightly calcareous, grey to grey-green (Smirnenski and Florentina formations)Marls and clayey sands (Cartajani formation)Clay and marls with limestone and sandstone intercalations. On Romanianterritory - sandstones, limestones and marl clays (Krivodol formation)
4,0 km0 1 2 3
alQP1
alQP2-3Alluvium, Middle Pleistocene T7, T6, T2alQP2
Alluvium, Middle-Upper Pleistocene - T1Alluvium, Holocene - T0alQhAeolian-eluvial, loess-soil complex, Middle-Upper Pleistocene - OEAL, T7, T6, T2eol - elQP2-3
Aeolian-eluvial, loess-soil complex, Upper Pleistocene - T1eol - elQP3
Quaternary boundaries:2,59 - 0,78 Ma
0,78 - 0,12 Ma
0,12 - 0,011 Ma
0,011 - today
Lower PleistoceneMiddle PleistoceneUpper PleistoceneHolocene
Civil contract from 30.04.2015Development of a unified conceptual model of the geological-tectonic,geomorphological and hydrogeological conditions in the 30-km zonearound the Radiana site on Bulgarian and Romanian territoryStage: II and III
Principal: SERAW
Geological profile across the 30-km zone of the Radiana siteScaleh 1:100 000, Scalev 1:1000
Composed by:
Drawn by:
Prof. Yordan Evlogiev D. Sc.
Evlogi Evlogiev
July 2015Appendix 2
C
C
L1
