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