1015202505
GEOLOGICAL MAP OF KOSOVO Scale 1 : 200,000
7420000 7430000 7440000 7450000 7460000 7470000 7480000 7490000 7500000 7510000 7520000 7530000 7540000 7550000 7560000
20°0'0"E 21°0'0"E
55 γδNmh 0 Regional Geological Units of Kosovo Scale approx. 1 : 1,200,000 Geotectonic Units of Central Balkan Peninsula Scale approx. 1 : 5,000,000 0 0 0 0 0
0 mPZ2 0 9 9 7 7 4 4
C
A CVBK - Badofc/Kishinca Cenozoic volcanic complex CBDR- Drenicë Cenozoic basin TKO- Koritnik Triassic unit IN σJ2-3 N RP
CVKB - Kopaonik/Belobërdë Cenozoic volcanic complex CBMI- Mirushë Cenozoic basin TMO- Moknes-Alpet Shqipetare Triassic complex αEo-Nm ER A
CVMB - Majdan/Braine Cenozoic volcanic complex CPA - Pashtrik Upper Cretaceous syncline TKR- Çiçavica Triassic unit 50 C o A T CVMS - Mitrovicë/Samadrexhë Cenozoic volcanic complex CPG - Pagarushë Upper Cretaceous anticline TKU- Kutlovc Triassic unit R Nm P H CVNK - Nosale-Kllokot Cenozoic volcanic complex CCA - Carralevë Upper Cretaceous unit MKO- Kolashin metamorphic unit 35 vs σJ2-3 A I
o 20 T o 20 H A CVRB - Rogoznë/Bube Cenozoic volvanic complex CJE - Jezerka Upper Cretaceous unit MSH- Sharr metamorphic complex o 40 o I
C A N CBDU - Dukagjin Cenozoic basin CKC - Kaçanik Upper Cretaceous unit MST- Shtime metamorphic unit o N A S CBDG - Gjakovë Cenozoic subbasin CZU - Zubin Potok Upper Cretaceous unit MGA- Gadima metamorphic unit L S I TRANSYLVANIAN M CBDP - Pejë Cenozoic subbasin CVT - Vardar Lower Cretaceous flysch trough MKC- Kaçanik metamorphic unit λEo-Nm M I O A
CBDS - Suharekë Cenozoic subbasin JBR - Brezovicë Jurassic ophiolitic complex MRU- Rugovë metamorphic unit N BASIN N N S U o E PANNONIAN BASIN N A CBKA - Kamenicë Cenozoic basin JGJ - Gjakovë Jurassic peridotite complex MNB- Novobërdë metamorphic unit S I N - U A αEo-Nm P T T H P CBKM - Moravë Cenozoic subbasin JGO - Golesh Jurassic ophiolitic complex MKU- Kurolai metamorphic unit vpEo-Nm A N A A αEo-Nm P
75 30 25 U
Szeged I R o 50 o O E CBKK - Kriva Rekës Cenozoic subbasin JKZ - Koznicë Jurassic ophiolitic complex MJK- Kopaonik metamorphic footwall unit o vpEo-Nm N o M G (! S CBKS - Strezofc Cenozoic subbasin JST - Strofc Jurassic ophiolitic unit DA - Dardania massif (Serbo-Macedonian massif) S I -
N
35 AI T
80 T F CBKO - Kosovo Cenozoic basin JLE - Leposaviq Jurassic ophiolitic complex N E o o U 75 O L o 45 aQh M I o I Y CBPO - Podujevë Cenozoic basin JRA - Rahovec Jurassic ophiolitic complex νJ2-3 FER Sibiu 0 I 0 AL S
0 80 T 0 E C 0 0
o M (!
0 J2-3 λEo-Nm 0
σ 30 H
8 o o 35 8
7 7
o C
JLE 70 26 Z 4 4
o Pleistocene River Terrace of the River Sitnicë / Sitnica. G 35
Nm ET O
o35 vs ICU
o M
A
External Vardar subzone (EVZ) N
CVKB E 35 o20 R βJ2-3 45 σJ2-3 CUM
o BI
J2-3 80 o Beograd DANU
Drin-Ivanicki element (DIE) vs 45 P o o
Central Vardar subzone (CVZ) αEo-Nm o 55
G JLE λEo-Nm D W (! A
o 30 40 50 U E D
SJ2-3 E o R S
o T R T EEP
CVKB M E IN T CARPATHIANS FORED
60 20 R
CVRB I - I
h 20 T N I C o 55 V o O H
o O A
U o R
20 o P h σJ2-3 55 sKcn-mE 45 - H N
60 o J2-3 I M 35 vs 48 E IO C O (!
80 vsNm 70 A L
o D K
o o 75 S I
h60 45 o T Leposaviq/Leposavić o I East Bosnian - Durmitor zone (EBDZ) MJK 45 A T E o o o βNp L E Bucureşti J2-3 50 B B - MKO ν o 35 M R L O vsJ2-3 Kcn-mD SJ2-3 (! A E CBPO A S N B JLE o 45 40 C M
CZU TKU Internal Vardar subzone (IVZ) o 55 N o 30 Dardanides Cataclastic Bujanovc / Bujanovac Pluton T H SJ2-3 o 50 Sarajevo IA E A
CVMB (with Pegmatitic Veins and Schlieren). I N K MOESIAN PLATFORM o 45 o A N JST CVMS o o 85 R o 47 Z T mPZ2 70 N L
vpEo-Nm 80 o 45 O A h o 45 o !
50 o 40 - N ! Dardania massif (DM) o K I APZ2 40 o 85 H E Š
o !
65 50 λEo-Nm Kb-aC E ! T
0 o Eo-Nm 40 A 0 (Serbo-Macedonian massif) α o †
35 40 ! I 0 R 0 o 30 o 85 o ! D o βJ2-3 !
0 55 0 gPZ2 50 80 o 50 Z
0 28 N E 0
TMO MRU TKR h † mKcn-moE E o βJ2-3 45
7 o 65 o o o G ! FORE BALKAN 7 CBDP 60 60 D ! ! S Sofia
7 CVT O 7
CBKS o 60 ! o
4 55 o 68 34 V ! A 4 50 σJ2-3 60 !
CBDR h o o I ! 60 † o
o 55 I !
o o 32 ! ( STARA PLANINA ZONE 60 N N ! λEo-Nm o (
αEo-Nm 45o
DA ! R
I ! o
vpEo-Nm 55 50 o 32 A A Prishtinë !
CCA 20 70 C o o o
65 45 N !
!
CBDU CVBK h o25 o 37 o R Z
h 55 ! CVBK o 57o O MKU 40 o N S
50 νJ2-3 E ! 45 o ! S
CVT 35 33 I ! RED
CPG SJ2-3 ! E NA
JGO o o GO
MNB APZ2 40 ! o R
SJ2-3 D ! A CBKK o 48 ! h 55 ! R
CCA CBKO 55 gPZ2 Kv-hC B B o † λEo-Nm o 50 o A 50 E ! L
CBMI JKZ 65 (! O KA
o o ! N 45 M
o 50 46 ID
JRA MST 12 36 o o S ! - ES
CVNK CBKA 55 ! Skopje o o ë I M
J2-3 † vs 60 † j R
Miocene Tuffs with Bombs. oo e E h P 65 65 68 - D A
MGA o 70 σJ2-3 55 ra l A 70 55 o
o o 42 o 72 d a I S C 38 o ko rs T o † o e 50 h v A T E S s E V
MNB o 45 n
CBDG h fPZ2 40 ra O R A D RHO
CVNK † o 60 o 38 o 52 T DOP 25o 40 E M
CJE o o 60 P N R O AS
85 o SIF
o 39 o
H O D N mPZ2 o 45 H JGJ 50 45 35 dQh62 ! K I CBKM o SJ2-3 60 o ( O P P A I N o K
o R L H A 45 o N " 60 E E R
85 40 I O I 70 o N "
25 o Tirana A T O
0 o 67 52 L o CBDS o † h ' 50 o
vpEo-Nm 75 o 22 o L E R A L Z 0 60 50 60 o S M ' 0 I
o † B A T O
o G 0 ° o H MSH CKC o o E o
60 50 o L R B A MKC 50 80 58 60 N ° 3 68
T A O o B o o o I S
vsJ2-3 3 o
65 45 40 † o E 4 37 o 66 A E
o 55 72 o A N Z N R S 4 45 h JBR o 60 h P
0 CPA o C O A 0 λEo-Nm lKcn-mC o U I I
0 o J2-3 N 0 67 70 β 45 85 N - H N A F MKC h o †
0 Kb-aC L 0
sKcn-mE h 76 o IO Ç N C 45 o 85 1 50 o I E 0 52 J2-3 o 54 75 A H 0 o 30 o vs o I 60 o
6 6
o 25 o 35 Nm 72 N N U
o 50 D M o o 16
7 35 7
75 55 20 52 o K
70 o 75 I
4 Z 4 o Ophiolite belt (OB) h 82 o 45 A A o TKO h o 30
O o o E A
K 23 s sKmD o 35 N S o Kb-aC
50 60 o 62 48 N L
o 70 r 40 60 75 80 R
o 10
o S
45 σJ2-3 h E I
20 h S o 89 o 45 o Z
25 75 h
o 38 dQh U Z I
42 o
o O F o
o o h o h o J O
o 45 30 45 † 48
70 20 o 60 66 A
45 o 55 o 56 N N
o o 55 o 50 h h o
h 58 o 70 67 44 o 20 h E E
39 47 o SJ2-3 -
o 48 35
o o h ( o 40
36 o G h 40 o 50 o 85 o 40 25 40
Sharr - Korabi zone (SKZ) 40 h o S
47 o 50 40 s 50 36 38 A o o 65 o
30 r SJ2-3 20 U h
h o
39 o 55 h o o V
40h 45 70
o
50 † B h 70 o h R
o SJ2-3 o † P o
35 o 60 52
50 o λEo-Nm h60 65 O h 30 55 E
o 42 h h
50 30 sT1-2 23 o mKcn-mE o
42 vpJ2-3 h 65 V L
60 o 85
20 o o 1 h A
h 45 45 O
h 45 o
o
30 o
h 65 72 60 Nm G Aegean Sea
72 o h o 72
44h sPZ2 30 tQp SERBIA 60 h h sJ2-3
o 47 o o Z 42 o O
30 50 40 Adriatic Sea h o 45 λEo-Nm 30 30
h 40 o 80 25 h O N
45 o o o
o
57 h 88 o 75 I
60 o o 35 o N h h 25 47 A
45 50 o 80 58 35 N
h E
o 30 50 o † h 25 65 o 40
h 60 25 J2-3 Z 35 β o
40 h 30 78 O
o o h
o N
o h 78 E ) h
h 30 40 30
h 52
30 o h h 28 o
h 45 52 h
45 50 45 75 h h 50
h 50 h Kcn-sD
h 50
30 o 22 o o o o 47 2
o 20 52 30
cPZ2 o vpEo-Nm 45 h o h T2
o h vs Np
40 66 46 o 45 36 80
50 h
50 h o 35 35
h 80 45 o 50 o
o o
o 45 40 h Podujevë/Podujevo h
o o o 65 o 20 h 82 h 45 50 75 25 o 40 o h
0 o 50 0 o 35 o 38 h 35 25 o
74 48 o o h 58
0 60 35 o 60 57 0 h o
cPZ2 35 80 h o
0 65 1 h 0
h tQp 78 40
0 80 o o 0 70 h Nm 50 o
40 45 h o 58
5 h h 5
o † h h 45 30 o 14 7 42 54 7 o o 65
4 35 o 40 65 70 4
h o
35 40 o 35h 45
60 o 62 20
h 60 o 35 10 o h o h 50 h
sJ2-3 30 o o
h 37 50 50 o
o 42
48 o
40 o Kcn-mE 55 o o fy h
30 sKmD o 20 60 o 51 o 45 50
h o
o h
76 45 sPZ2 12 o 40 o o
o 55 52
o 42 30 o
85 50 20 45 o Mitrovicë/Mitrovica 16 o 40 o
o lT3 o
60 58 o 15 28 h44 35 65 h o Kb-aC 30 o 66 h 75
h o 70 40 15 h
o h
h o
† 40
o 25 60 o 35
60 cJ2-3 o 70 o h o h
o 80 50 o 50 o
o o 52 o
o αEo-Nm
35 65 50 25 o 20 70 2 45 h 52 r fKcE
60 o lQp Qp o t o 56
o 45 Np
o 45 s 35 30 o o o 38 B h 40 h o 80
o 56 65
70 42 o 70
SJ2-3 o
55 o o h o
o h 70
h Qh
h 45 o 55 30 40 o a
o sJ2-3 15
60 o 40 o 84 Kv-hC s
o 38 15 vpEo-Nm o 56 38 o
h 72 o o
o 60 s r o 40 h
40 40 o 35 30 60 o 15 gNP r o
o
o 30 h o 63 68 o 65
70 o o o 52 h
o 45 h 56 50 50 30 h o 50 48 35 15 20 o
h
o o
o
40 o Qp o o † o 50 40 40 Kc-tD o t
30 60 o 80 55 h r
o o 45 50 h o o 60 †
35 s 30 30
o o o
50 o o 50 Qp 65
h 50 40 Qh t
h 50 30 o 30 T2 15 d 25 45 vs o
o o
h h 60 o 50
o
h 50 50 55
o Vushtrri/Vučitrn lKcn-mC o o 33 70 o
o o o
h 45 o 50 MONTENEGRO 45 50 o 50 o
60 65 15 15 h 40
o J2-3 50 64 o 84 40
h vs 30 o
o o 45 o 25 o
30 38 o o o
45 45 10 35 25 o 30
45 h 35 o o
o 15 o
45 o o 60 o 70
h 50 vpEo-Nm
28 o o o o
lT3 o
15 o
20 50 45 o 40 35 o 45 20 60
45 40 o h o 30
o
o o
0 0 o h h 64 o 40
55 2-3 40 o 50 o
o 55
0 55 30 o 15 75 0
o o
o 35 Nm o 45
0 Qp 2 0
o o t h
o o o 45 45 30 35
0 sKcn-mE 0 40 o 45 20 Np 4 o o 50 4 o o smJ2-3
ocJ2-365 o 30 45 45 o o
7 o 50 60 7
o 40 45 o o 68
4 o 4
45 45 50 o
36 35 o o 70 12 o o o 10 44 20
35 o
o 2 o
40 50 o 45 o
Qp 30 l o o sEo
o o 75 o 30 2 o 1 o 40 25 10 36 Np 52 o o o
42 lQp 10 50 45 o 65 SJ2-3 Np o
30 h o 75 80 o
o s o 70 Kv-hC o 45 o o o r 40 Eo-Nm
48 60 lQp Qh 70 50 α
5 o p
o 36 o 70 o o o 5 2
o 54 vsJ2-3 o 4 o28 o50
o o kEo o 10 o 22 o
40 o o 70 †
o 10 35 65 40 Kb-aC
o pQh 50 25 2 o 40 o 50
45 o h
vsT2 vsT2 30 20 15 o lEo 35
50 o o o o
o o o 8
vsT2 o o 30 30 o 50 20 40 o
15 2-3 h 30 o
o 30 o 40 50 o 25 High-Grade Metamorphic Rocks (Migmatitic Gneiss) in the Kaçanik s
25 40 o Nm 5 o Qp 40 o 15 55
5 l Á o o o 56 s 56
h o Metamorphic Unit. o 20
o 22 o 76 o o 56 o mKcn-mE 28 o
aQh 10 h 1 40 o o
35 25 45 o 35
10 o 52 h
Np h
o
lT2-3 o 35
5 58 o o kT1 10 10 o lT2-3 o o o
35 o dT1 36 2 o 28 50 o 56 o68 70
dT1 5 Kcn-mD
o tQp o 8 o h Np o 5 72 65
10 30 o o 76 o 55 65 gNP o 45
12 o 60
10 o o SJ2-3 o
o33 o 25 o 17
o 30
qPZ2 o 40 60
36 10 h
35 12 o o o
h
h o
10 o kT1 o
25 o 35 10 o h
h 20 Kc-tD pQh Kv-hC o55 o 85 2 70 o 30 o h vpEo-Nm 40 Kcn-mC o o sm 40
h cQp 60 30 o20 25 o 68 85 sEo h
o Qh 60 o
0 o30 d o 75 0
40 2 o o 25 28 † 20 o
0 fPZ2 30 15 0 o mNP
Np 55 o 0 o 40 0
36 o 7 vsT2 15 o h24
0 SJ2-3 32 59 30 0
40 o
h
48 o
3 o o h 75 45 53 42h 3 o 75 o o 30 50 o mKal-cC o o o o 30 7 27 Qp 68 7
36 50 37 l 55 o o 4 65 h 4
o 80 42 o o
5 10 o 20
35 44 o 10 46
o h o
40
o o 65 kKal-cC 40 25 o
lT2-3 o 75 mKal-cC 30 o o o o 60
30 30 †
o o o
10 o o
o 38
o 12
45 o o 63 o
38 o 8 25 35 50 gNP
o 30 35 o 40 o 80
o o
o 57 65 h h 50 o o h o
10 o h o 25 o 65
gQp o 38 o45 25 40 35 30 o 45
o 10 o 78 25 o o 30
35 55 40 Kcn-mC o h
o b 50 2 o kT1 †
o
h o
s
o h 48 65
o 2
10 40 o 25
45 Qp 10 10 o 25 sEo 60 h
l s 30 65 o 33 40 o h o h o
o 65 o
r kEo r o o
o o 80 o 35 SJ2-3 o o 22 80 42 40 h ANP 45 Á
o 50 42 47 41 r
vsJ2-3 35 56 o o o o o 22 o 76
15 50 10 o 70 26 o
h o 42 † 38 1 30 h h
6 h o
o 15 o SJ2-3 35 0
Nm o 25 h
o 35 h o o
s Np sJ2-3 o h 5 o 50 kKal-cC
o o 25
45 r o o 60 32
2 35 80 25 h
aQh o 40 o o 30
o Kc-tD 58 45 o 32
o 45 o †
25 75 o 38 h 35 h Np o 38 h 48 h 1 o †
1 15 55 40 o 18 65
h 10 o
o
Np o o 35 35 o 30 38
35 Np 30 o 60 30 o o 25 58 h
o lKcn-mC o h 34
o 38 80 h 60
50 30 J2-3 56 o o 30 45 σ h o o o 45 h o
Qh o o 30 50 42
dT1 o p 50
o o
25 60 30 o o
65 †
o h
o cJ2-3
lT2-3 70 h h
o h o
45 35 h MNP 55 o 65 o
26 o 60 h 70 o 10 o sKmD o o 60 o † mNP h 15 Qp 40 o 80 70 40 h 46 35
b o o 50 25 h 50 80 s
30 40 h o o 30 h
o h o h h 44
25 10 14 h o 25 h 68
o 38
s
o 50 60 20 h o 65 o o 1 h
26 38 o o 70 40 40 h
15 80 h 30 70 42 h
o o 40 40 Np APZ1 mKal-cC 40 35 48 38 h
h 20 h
o h o 35 o o 43
40 o50 Pejë/Peć 30 o o 50 Prishtinë/Priština 45 55 50 2 gNP o o o 45 35 o 60 o 37 h o † 45
20 o 60 60o h
o h lEo 30 h
2 o o 40 s Qp Kcn-mC 70 45 h h vsT2 lQp l sm 70 80 h gNP
o 70 r h h 56
s 42
o h 70 o 15 35 70 75 h Á
vsT2 Np h o 70 o 70 h 80 35 57 38 50 h s
Qp Nm h o s h
t 30 h h MNP
50 o o Á o 60 44
Qh 35 h s o h † 70 h 38 50 IT3 d o 60 60 55o o 70 70 25 60 75 48 40 h 60
h h 25 o o h o 38 h
45 cT1-2 h
o 70 53 J2-3 o 1 β h Qh o o d o 52 o
ST2 o o80 o 70 80 45 43 h h
40 AJ2-3 h h
s Np 35 40 h 60 45
o h 40 h r 70 45 40 46
60 h 25 h 70 80 80 34 o h 22 30 o 32
tQp 30 o o γPZ 40 80 o 30 h fPZ2 o 65 h
o 80 50
0 o 65 h 0 h o 50 o 1 h h ANP γPZ 30 gNP † 0 h 0
o 20 o sJ2-3 80 30 28
r
0 Np h 0 s h 36
h 60
o 30 h
10 smJ2-3 o
r sT1-2
0 55 Qh o 50 35 2 0 p o
65 50 h h o 20 35
h s h h 54
2 40 2 36 h37 o 20 o o 25 kKmD h h 60 lEo
35 50 85 o 50 h h
70 h o o
7 h 80 h 7
70 h γPZ 50 h 34
o Nm 40
4 Qp 25 h30 70 48 4
cPZ2 b h h h h
h 35 30 o o
dQh 25 aQh o 27 42 74 60 65 70 40
o AJ2-3 56 58
h h 16 50 20 h h h o h 20 o 35 cPZ1
40 h 1 o SJ2-3 60 sPZ1 o o 35 h 70 h o 60 h h o 50
30 35 Np o Qp 60 σJ2-3 60 o l
r h 56
T2 o 70 β h
o 75
s 60 h
1 s
o 25 70 qPh Z1 42 20 r o 50
r 42 35 o h 45 35 o
20 Np 40 70 o 30 o MNP h s 35 60 o 25 h 50 o h
o 15 20 o 80 38
o 70 o
o lT2-3 45 o s cJ2-3
o 70 20 57
60 h o 36
o o
r o
dT1 o 55 h 40 30 25 h
o 40 APZ1
h † o
25 o o 50 40 h SJ2-3 60 vpEo-Nm h 60
50 o 35 18 Kv-hC 15 h o Qh o h d o
γT2 h o o h42 30 85 60 50 30
o 25 o 25 h
h 20 h
35 5 12 o 80 60 MNP
25 60 35 65 80 h
Kcn-sD o h
h h
h 80 35
40 o 70
lQp h h 50 o
o o o 45 28 40 60 αEo-Nm cPZ2 58 h 2 SJ2-3 o
bQp 16 28 h o
15 o 18 h o o
Np o 70 1
40 h o 50 70 o h 40 h
o 27 50 o sKmD o 70 Np MNP 70 65 h 50
o gNP h
85 60 h o 35
lKmG 35 αEo-Nm h 15
65 o o o h 28 † 70 o 25 70 60 h 2 o 12 o
o 20 ρJ2-3 Ks-mG 20 o pQh 75 γPZ
h o 20 70 65 kNm dQh 37 o o mKal-cC h
o 65 o h h 35 σJ2-3 75 h
18 o 70 50 2
1 o
h
1 sKmG 25 30 25 h 78 30 72 mNm Qp mPZ2 o 32 kKal-cC g sT1-2 o Np o o 60 sPZ1
sT1-2 83 o aQh
h
Np o SJ2-3 o h 50 8
h20 h σJ2-3 sKmD 82 80 γPZ 35 h 12 lQp 80 h tQp
h 25 25 55 o 60 70 82 h 50 cPZ1 o
35 o 46
o
s o
o h
11 r 30
45 o o 55 o 32 h o h 26 o h o Kcn-mC 70 lKtG h osm82 SJ2-3
βPZ 25 20 50 60
o o 30 h
60 Qp 45 h
g o 20 o
h 30 h 60 40 28 h h
h lKcn-mC o 76 2 2
o 30 45 65 h
cPZ2 pQh νJ2-3 30 h sEo h 50 mNm
Ks-mG o o 0 0 Qp 20 h b 55 s dQh 75 r 0 0
o 87 80 PZ
o80o o γ o
o 50 o 86 60 15 10 o
0 65 15 70 0
o 1 o 15 h 15 o 0 0
60 o
Qp o 13 r h h
g s SJ2-3 Np 10 o 1 J2-3 15 20 80 55 1 vs o
PZ o 20 75 o 50 h 52 2
ν h
7 35 h o 80 12 7
1 o h PZ o
o γ
PZ 75 h
β h 60
o
4 sNm 4 h 60 50 † †
Np 14 γJ2-3 h o
20 65 60 80 o
lKmG 50 βJ2-3 70 50 o 65
o
h 70 70 1 54 h
h
2 o
h
o r o
Np h 45 o 40
gQp Np 20 tQp 35 40 s
o h h 32 o 40 10 o sT1-2 MNP
o lKtG 14 fPZ2 Kcn-sD 80 o o
o 50 h 65 85 60 † h 30 h h o sKmG o 75 h 2 40 20 lQp 60 h42 o 40 o 50 h o 65 mNm o 26 60 70 55
h sJ2-3 MNPh
2 o 25 o
50 Np o h25 fPZ2 Qh 30 † o 80 d o 15 65
25 o h 84 cJ2-3 50 h
40 60 h h 70 h
Qh h h h h o o 50 30 h o a o 46 80 45 70 νJ2-3 2 h80 smJ2-3 τEo-Nm ANP43 K1G h 70 lEo
gQp σJ2-3 12 h o 70 2 aQh o 80 h h o
o 50 10 25 h50 70 80 65 mNm o h 15 J2-3 h 50 γT2 80 h50 ν h
sKtG o h o smJ2-3 60 sPZ1 Á s
βJ2-3 30 γPZ 30 40 70 20 h gNP s
Ks-mG lQp pQh h 65
† o 68 50 h o h o o o 80 65 h
5 o 60 h 30 h 35 s Qh SJ2-3 h h h h h 30
20 d 60 80 40 70 h sγPZ o 1 o 42 80 o 28
50 h 80 o 80 o 65
SJ2-3 σJ2-3 h o o 80 48
15 Np kKmD 60 o 70 h 35 80 lKtG h
SJ2-3 o o o 35 h 64 h o
ALBANIA 80 o dQh qNP
o 16 10 46 h sPZ1 50 o 80 70
Á
gPs Z2 75
o s o h
o 60 cPZ1 †
20 o o h h 40 † o
25 36 o 28 o 45 Qp 70 h 37
o lQp 10 d h sT1-2 75 70 37 o o 15 25 60 o 50 βJ2-3 o 50 Gjilan/Gnjilane h o 25 o o o 60
tQp νJ2-3 h 50
20 25 qPZ2 h 2 qNP cPZ2 h 70 h 70 o o o25 15 dQh 30 80 o 80 sNm 30 2 o25 o 16 dQh 28 h70 νJ2-3 h o 34 o 50 o h γJ2-3 0 J2-3 0 Np 30 o σ 16 o o35 85 85 80 mKal-cC γPZ o h 0 tQp ρJ2-3 22 o † 60 mPZ2 h 50 h o80 70 0 0 o o 45 0 20 o
15 o 75 † 40 50 50 80
0 lT3 h h o 0 Qh h o
o d o h
15 o J2-3 10 70 20 o γPZ 0 5 vs † 70 0 60 h h aQh o lT2-3 o o 40 h h 50 h 7 60 o 7
o o 60 † h
o o o 35 † 32 30 h 70 h 60 4 70 h 72 4 25 15 55 o 20 40 h APZ1 44 o 65 o 78
35 h 70 85 o h
30 8 o 36 † Kcn-sD h50 60 o 60
25 40 o h
Ks-mG o o † o 30 65 h 55 † o o sKmD 70 o 85 o 80 80
o h
h
10 40 h h
40 70 h
sT1-2 lQp o smJ2-3 h h h 25 h 70 o 60 52 41 o 40 h h 40 νJ2-3 85 γPZ
10 40 25 h 85 h o 70 † 47 o o o o 60 35 fPZ2 h o o 18 80 o
30 35 o 80 h 56
o 30 Kc-tD 80 o o 40 50 o 57
o † h 30 47 75 h
dQh 70 h Eo-Nm h
18 o o τ h
Qp o o 30 h 80 79 62 35 ANP
l o45 30 o h 8 80 † o h 45 o 70
20 lKtG 35 1 h
o o 25 80 h80 64
35 o kEo o o h pQh o 50 70 h h 35 2 σJ2-3 gPZ2 h h 51
o 60 30
Np sQp 65 h h45 70 66 o sT1-2 h 65 50
o 12 o h 70 2
K1G 10 h 40 60 h50 h †
32 r h sPZ1 sNm
12 h h h 10 42
o 60 Á 45
o 65 44
o vsJ2-3 1 νJ2-3 o r 42
20 h25 o h h
2 h 30 h 60 Np dQh o 70 o h o 39 h 30 48 h
Np 25 33 h vpEo-Nm 57 62
o h82 o 40 70 h †
Gjakovë/Đakovica o 38 r 25 cT1-2 70 h
o o 63
35 s h 30 APZ1 s
h 50 2 62
h
h cPZ2
22 2 80 cPZ2 h h h r
o † lKtG o 15 50 65 o
30 15 80 h mNm Np h h lQp 2 49 h
22 h25 h Kcn-mD mNm † 70 o
32 o 55 70 APZ2 h 50
50 o
o40 75 h 48 h 40
80 h † 45 o h γPZ h
r 80 58
h h
35 cT1-2 r sKm40D
†
o s 45
† 80 Ferizaj/Uroševac o 25 o o
o 30 h
40 h 50 55
h 35 r 62 h 60 vpEo-Nm 0 h h 80 40 0
Á h pQh o
0 85 0 h 40 35 r o 12
0 σJ2-3 Kcn-mP aQh 0 2 h h 50 o 0 vsJ2-3 0
KtP h 70 o 80 o 9 9
Np 20 h †
20 s cT1-2 o 80 o 6 o 8 Kcn-mE 6 Á h
2 50 h h 60 35 55
4 s o 70 4
60
h 60 80
h
Np o Qp 1
h28 o l o 10 † h o80 80 kEo
Pliocene Fine Sand with Thin Gravelly Intercalations and Lignite Seam 80 1
2 lQp 62 smJ2-3 Np AP50Z2 pQh lKcn-mC h 60 sm
Np 53 80 h 45 J2-3
on the Top. †
10 h 50 o
o † o o mPZ2 o h fPZ2
20 60 Eo-Nm
35 aQh 50 o τ h h o
8 80 20
KaP 50 pQh o
35 h Kcn-mD 80
A 20 o h 1 o h h o o βJ2-3 2 40 h45 h kEo
Np pQh 50 40 h70 vpEo-Nm
67 r 1
σJ2-3 lQp lQp s s 40 h Á
36 50 70 h80 s Np o
ρJ2-3 aQh 50 cPZ1
h
h 1 h 70 40 2
o o
25 h
27h
SJ2-3 h h mNm lEo vsJ2-3
o 50 20 o smKcn-mC 45 s
o o 60 60 80
40 80 50 s 60
s o o 25 o
h h 55
h h60 h qPZ1 o 70
h 60 r 75 o45
25 45 50 o o h o30 25 85 h o ρJ2-3 o h 30
νJ2-3 25 o o h lT2-3 70 h50 1
25 50 lKcn-mC βJ2-3 o65 o h Qp
Map Description 30 25 o25 h sPZ1 20 Np l 1 1 h60 h γδJ2-3 o 40 40 o 50 55 o45 o 70
20 o 28 h lEo kEo o
o 50 h 60 60
25 SJ2-3 h o
Qh 60 h o 60 o
p o lQp h 25 cPZ1
Ka-cP o 35 40 h 50 h50 fyKcn-mE h50 πEo-Nm
40 h80 h 1
35 45 h30 75 J2-3 70 h σ o J2-3 h γδ
o 20 o lEo 60
o 35 Qh o 50 o
Kosovo is characterised by a variety of geological formations ranging from old crystalline Proterozoic to youngest o p 50 45 h 70 18 o
KtP 25 30 80 o 65 Triassic Metasandstone (Left Side) and Metadiabase (Right Side, o s h
2 h h h o qPZ1 45
0 Kcn-mP o 2 50 in the Foreground). 0 Np lT2-3 h 0 dQh 70 r 0 Quaternary age, comprising sedimentary and magmatic rocks together with rather less frequent metamorphic o 20 Np h60 νJ2-3 o 35 h 0 35 23 15 h25 70 h60 νJ2-3 0
0 o 0 o 15 15 o h SJ2-3 50 mPZ1
8 rocks. o h βJ2-3 o 8
o 35 15 30 1 6 20 o 25 50 Kcn-mE 6
o h
4 o Np 4 h 70
o 25 h gQp o
20 40 15 o 10 o J2-3 o 80 γδ
20 o 30 h67 h55 h40 60 65
lT o
o 15 s h cPZ1
25
76 h 85
The oldest core of the Balkan Peninsula is situated within the Circum Rhodope belt with medium- to high-grade- r 30 lT h 60 h h o AJ2-3 h fPZ2 25 50
25 65 sQp 30 h o o o
h h40
metamorphic crystalline units (Dardania massif / Serbo-Macedonian massif, Rhodope massif, Geticum etc.) and 15 h 50 h20
50 Qh 45 h 60 o 50 p h o h
h h 40 h70
25 KcP o 25 40 qPZ1 65
o 20 50 h o h the marginal zones of the Pelagonian massif. As a result of Palaeozoic subduction and Hercynian collision, these 15 h o
lQp 58 βJ2-3 30 SJ2-3 h60 h25 65
25 σJh2-3 σJ2-3 lT2-3 sPZ1 o30 h50 o
h 40
o 20 50 45 25
Proterozoic and Palaeozoic continental massifs have been merged into a single continent. The Triassic o h 87 h o
cPZ1 lT o
25 Prizren/Prizren h SJ2-3 h 40 o44
intracontinental rifting led to the break-up of the Palaeozoic continent and to a different evolution of the 25 70 h80 80 40 Kcn-mE o
15 o o 42 smJ2-3 h45 h h o h60 o
KtP h50 45 30
h 30
o h 50 gQp o 40 30 h40 h
microcontinents. Later, parts of it (e.g. the Dardania massif / Serbo-Macedonian massif) were tectonically 20 h 70 45 25 50 h gPZ1 mPZ1
h 80
h 50 h
h60 h 50 h bQp AJ2-3 h 45
15 o 70 35 h 45 20 60 o o 25 2 h 60 30 40 h h
h h h 50 45
separated and structurally incorporated into the Alpine evolution. Np lT2-3 h o 65 o
o o 15 lT2-3 h55 o
20 40 50 σJ2-3 40
o h55 50
25 h 85 h
h h o 60 lT 15 dQh h h60
17 o h 22 h
The Vardar zone represents the most mobile zone of the Dinarides-Hellenides. This lithologically heterogeneous o 20 26 45 40 10 o40 h o
o
o cPZ1
25 30 h gQp fyKcn-mE o 60
o h h
and tectonically complicated zone was built in the Upper Jurassic and Lower Cretaceous after the stable 17 50 lT2-3 30 APZ1
h
o h 35 βJ2-3 25
h 35 h40 smJ2-3 Qp 70 o 30 h o75 h 45
Palaeozoic crust broke apart and a system of troughs and barriers was generated. In this area, shallow marine t h 40 h νJ2-3 h65 o
40 30 60h 60
15 h40 40 h h
0 limestone can be found up to the Upper Triassic (marine carbonate platform). The separated Dardania massif / o20 0 70h gQp
0 o 70 dQh h o h h30 0 o
25 h h 15 30 o 0 35 Qh 65 35 0 h 25 d 20
0 h 45 o o 0 Serbo-Macedonian massif became a mainland, thus dominated by erosion. Other areas of stable continental crust h o
7 SJ2-3 7
60 40 h lT2-3
6 Qh lT2-3 40h 70 dQh 6 p h 4 35 30 4 h h
already started to break up during the Middle Triassic age, which led to the formation of small troughs, h10 15 h h cPZ1
h h 45
35 45 45 h
30 27 SJ2-3 o
10 h h h 55
accompanied by more or less intensive rift volcanism. 40 30 35 25
70 h
o h h mPZ1
30 o
o h 3 h h
h γPZ 15 h 40 60 Nm
65 o h 45 26
25 h 30
28 h lT2-3 h 60 h h The Inner-Dinarides trough, which is located southwest of the Vardar zone, also got subdivided into barriers and o 28 43h h 60 dQh h30 20 SJ2-3 fPZ2 h25 o cPZ1 basins since the Triassic, so facies differences have to be looked at in detail. The occurrences of volcanic- 50 50 fPZ1 75 45 o h30 h55 qPZ1 o During the Neogene, fracturing and subsidence of intramontane basins became most important. On one side, the h
sedimentary series starting in Middle Triassic age are a common feature. Basic and ultra-basic magmatic 35 o o20 20 o southwestern areas (Albania) have been influenced by marine ingression during the Oligocene and Miocene. On lT2-3 h30 AJ2-3 activities have probably been connected to the creation of deep fault zones (rifting) and the formation of the first 30 h40 h35 πPZ
o sPZ1 o65 the other side, the area of today’s Kosovo was dominated by silty-clayey lacustrine-terrestrial sedimentation (with
oceanic crust (opening of the parts of Tethys ocean). 40 h o o 25 40 45 35 7 h pQh 30 h h important lignite deposits) mainly during the Miocene and Pliocene. h fPZ1
A separate barrier with Upper Palaeozoic rocks exists between the Vardar zone in the NE and the Inner-Dinarides 55 h35 MACEDONIA 25 h lQp 30 h24 J2-3 o
h40 o30 σ mPZ1 The gradual development of Cenozoic sedimentation basins ranging from the Eocene basin in the NE (outside o in the SW since the Triassic. The flanks of this barrier have been dominated by extensive gravitational marine o 40 30 aQh sPZ1 lT2-3 SJ2-3
o 38 Qp Kosovo) to the Pliocene basin in the SW was accompanied by intensive post-collisional andesitic volcanism inside o h g h75 sediment transports directed towards the Inner-Dinarides trough. Later on, after folding and sliding movements, 15 35
25 h γPZ o40 the Vardar zone. The volcanic activity in the Kosovo area, which started in the Oligocene and had its main phase 0 this barrier probably formed the Drin-Ivanicki element. o νPZ cPZ1 0
0 35 fPZ2 55 during Miocene, also brought up granodioritic masses. The sedimentary basins are masked on the pre-Neogene 0
0 PZ 0 gQp h lT2-3 h ν 0 0
6 structures trending preferentially in NW-SE and NE-SW direction. Their activity continued until the Quaternary. 6 6 The Vardar zone (Vardar ocean) and parts of the Dinarides Zone (Mirdita respectively Budva-Pindos oceanic h35 h55 qPZ1 6 4 40 4 45 h h 15 basin) are regarded as an oceanic crust area, divided by the Pelagonian platform. The Middle to Upper Jurassic
o h45 The youngest tectonic activity generated vertical movements, uplifting and subsiding of separated blocks. The ophiolites comprise a thick sequence of ultramafic, basic as well as basaltic rocks, which possibly syn-kinetically 35h lQp qPZ1 central depression (Pejë / Peć – Prizren / Prizren) is a downthrown block (the total subsiding exceeds more than
(in connection with the sea floor formation), but mainly post-kinetically (in connection with later tectonic ζPZ h40 thousand metres), surrounded by upthrown blocks, which still ascend with an uplift rate of 0.4 mm per year.
60 transportational processes) have been serpentinised, mostly. At the end of the Upper Jurassic and the Lowest h
Cretaceous, the ocean was closed again. Early Cretaceous “pre-flysch” is composed of fossiliferous clastic rocks, πPZ 40h In the Pleistocene, the highest mountains were covered by glaciers. Their glacigene (moraines, lacustrine and h qPZ2 45 45
60 h
45 h which are unconformable overlain by Upper Cretaceous carbonate followed by mainly sandy-silty flysch h fluvial) deposits occur in southern and western part of Kosovo. River terrace sediments can be found up to 35 sPZ1 sequences. h hundred metres above the actual stream level. Deluvial debris, proluvial fanglomerates and alluvial sandy-gravely
πPZ 50 fPZ1
30 h deposits in the youngest valleys are of Holocene age.
h The subduction of an oceanic plate underneath the continental crust of the Carpatho-Balkan arc started in Lower h 80
Cretaceous. Hence, the Vardar zone ophiolites may be obducted during this process, whereas the Kopaonik ζPZ 50 The geological formations have been delineated based on the information shown on older geological maps. The h
N recent map features a unified legend of the geological formations, which was applied all over Kosovo. The legend block can be interpreted as the island arc, which was separated from the Rhodopes and Dardania massif / Serbo- N " " 0 '
h 0 πPZ fPZ2 comprises a stratigraphic classification of the formation (fill colour), as well as of a representation of the rock '
0 Macedonian massif by this marginal basin. These ophiolites were partly accreted onto the active continental 50
0 0 o 0
° 28
0 20 0 ° h
2 h
0 20 25 0 margin and covered by rudist limestones and flysch sediments in the Upper Cretaceous. The formation of flysch 25 lithology / genesis / petrography / alteration (fill pattern). The classification of the geological formation concerning 2 0 0 4 o o 4 5 h30 5 6 sediments in the Vardar zone is proven since higher Lower Cretaceous. In some areas (only outside of Kosovo) stratigraphy and lithology can also be derived from the rock abbreviation used on the map. Beside this, the map 6 4 o 20 4
γδPZ πEo-Nm
basal parts of flysch are interlayered with basalts and rhyolites and intruded by anorogenic intraplates granites. cPZ2 contains information about the main geological boundaries and the most important tectonic elements. Olistostrome horizons are very common in Upper Cretaceous. o 30 o 30 o 30 h The map has been compiled in ArcMap GIS format. It is a feature of the GEO-Database Kosovo, in which more o 25 information is stored providing the possibility of combining various thematic information. For detailed information
Compressional tectonics due to subduction-collision mechanisms transformed the basins and platforms into fold 20
and thrust zones in the late stage of the orogenic deformation. As a result of the stable tectonic setting, all major 20 o 20 h see www.kosovo-mining.org. Available documentation and used literature can be acquired via ICMM. h gQp
49 qPZ2 Mesozoic palaeographical units turned into fold and thrust zones, starting NE to SW. o h19
o 24 mPZ2 o 30 40 Both, the appearance of the microplates together with the accretion of partly small terranes and the transition to h o 32 20
o 30 h Selected Literature and Sources of Data
younger folding towards SW are characteristic features for the Balkan Peninsula. By the end of the Upper o 25 o 30 cPZ2 s
gQp r
Cretaceous, in the Palaeogene, the subduction was followed by a continent-continent-collision, which led to 20 25 EOLOŠKA ARTA RBIJE
h G K SR S , 1 : 200,000 Beograd 1968, Zavod za Geološka i Geofizička Istraživanja, Languages:
h h
h βPZ o
strong collisional deformation, the uplift of the Dinarides blocks and the overthrusting of flat nappes toward SW. 25 47 30 20 Folded Upper Cretaceous Platy Limestone (Carbonate Platform). Rahovec Ophiolite Complex (Basalt Pillows and Plagio-Rhyolite). r Serbo-Croatian and French). h
This phase was accompanied by granite plutonism and andesite volcanism in some parts of the Balkan Peninsula s h h45 o 35 15 30 0 fPZ2 βPZ h 0 0 20 GEOLOGICAL MAP OF YUGOSLAVIA, 1 : 500,000 (printed 1971, 6 map sheets). 0 0 and metamorphism of some parts of the Mesozoic graben-sediments. The cumulative tectonic shortening of the † 0 0 14 mPZ2 o 0
4 30 h 20 4 6 6
crust has been estimated with 500 km. † o h h
4 EOLOŠKO EKTONSKA ARTA OSOVO 4 30 G -T K SAP K , 1 : 100,000, Zagreb 1974, Geozavod Zagreb, Language: Serbo-
36 h
PZ Croatian. The SW-vergent structures of the Dinarides were formed by geodynamic overthrusting of the geotectonic units 10 γδ
o 30 γδPZ
20 h gQp from NE to SW in the Palaeogene age. As a result, the Triassic East Bosnian-Durmitor zone is lying above the o OSNOVNA GEOLOŠKA KARTA SFRJ, 1 : 100,000, Beograd/Titograd/Skopje1970-1984, Geozavod Beograd/Geološki Adrian foredeep and the Dardania massif / Serbo-Macedonian massif pushed the Vardar zone against the qPZ2 20 45 Institut Beograd, Zavod za geološka istraživanja SR Crna Gora, Geološki zavod Skopje, Language: Serbo- h h
Palaeozoic-Triassic Drin-Ivanicki Element. The Peri-Adriatic Fault (PAF) is seen as the lateral shear lineament 30 1 : 200,000 h Croatian). fPZ2 70 between the accreted structural elements (terranes). h 0 5 10 15 20 25 GEOLOŠKI ATLAS SRBIJE (GEOLOGICAL ATLAS OF SERBIA), 1 : 2,000,000, published by Ministry for Mining and The low-grade metamorphic rocks, which are common in the Kosovo territory, have to be interpreted in the frame IMITRIJEVIĆ Kilometres Energetics Republic of Serbia and Geomagnetics Institute, ed. D M. D. et al., Beograd, 1994-2004, 16 of the extensive subduction processes. In general, the exposure of these rocks has to be connected to the map sheets themes Palaeogene phase of the orogenic cycle. Until now, their metamorphism age was interpreted as pre-Mesozoic, but more likely they are Alpidic. These units are fragments of older, metamorphically overprinted rock series of a THE COMPILATION OF THE GEOSCIENTIFIC MAPS OF KOSOVO – GEOLOGICAL MAP 1 : 100,000 – Description of the Map tectonically and palaeographically uncertain position. Compilation – Beak Consultants GmbH, Prishtinë, March 2006, 175 p. 0 0 0 0 0 0 0 0 3 3 6 6
4 Schematic Geological Cross Section across Kosovo Scale 1 : 200,000 4
OPHIOLITE BELT DRIN - IVANICKI ELEMENT VARDAR ZONE DARDANIA MASSIF A External Vardar subzone Central Vardar subzone Internal Vardar subzone B SW NE Gjakovë Jurassic Dukagjin basin Rahovec Jurassic Pagarushë Upper Mirushë Cenozoic basin Carralevë Drenicë Cenozoic basin Çiçavica Triassic unit Kosovo Cenozoic basin Vardar Lower Cretaceous Flysch trough Majdan / Braine Cenozoic peridotite complex Gjakovë Cenozoic subbasin Ophiolite complex Cretaceous anticline Upper Cretaceous unit volcanic complex 2 smKcn-mC Np Erenik tQp Proni i Beces Drini i Bardhë σJ2-3 K1G Mirushë Denac 1 Lumi i Sitnicës Lumi i Badlavës m asl 2 Ks-mG Np 1 m asl Np J2-3 dQh 1 vsT2 Qh β 1 lKtG Np tQp sT1-2 Np p mKal-cC vpEo-Nm σJ2-3 tQp lQp sKmD Kcn-sD smJ2-3 sKmD Kb-aC αEo-Nm gNP aQh aQh Np aQh dQh mKcn-mE 1000 KaP cT1-2 tQp 1000 v v v v Á Á Á Á Á Á V V V V V σJ2-3 V V V V K K K K V V V V V v vV Á Á Á ÁD ÁD ÁD D D D Á Á K K K v v K K v v v v v K v K V V V V V V V V V V V V V v v Á Á Á Á Á Á V V V V V KKKK K K K K KKKK K K D D D D D D D 0 v v v v v Á Á Á Á Á Á 0
K K KKKKKKK K KKK K K Á Á Á Á Á V V V V V V V V V V V V V V V V V V V V V V V V V V V V V V V V V V V V V V V V V V V V V V v v v v D 0 v v v K K Á Á Á Á Á 0 0 0
0 - 1000 V V V v v v K K D - 1000 0
0 K 0 2 2
6 lKtG 6 vsJ2-3 sKtG Ks-mG SJ2-3 smKcn-mC Kv-hC 4 σJ2-3 sJ2-3 4
Legend PALAEOGENE QUATERNARY Oligocene PALAEOZOIC CENOZOIC MAGMATIC EVENT TRIASSIC MAGMATIC EVENT
Holocene Upper Oligocene Lower Cretaceous Barremian - Aptian Upper Palaeozoic Oligocene - Pliocene Middle Triassic Geological boundary, observed
v K K K v
( ( v v v
( N ( N
£ £ £ . . . 2 8 8 8 Sandstone, siltstone, conglomerate, K K K Geological boundary, indicated v v ( ( v v v aQh Alluvium - gravel, sand, silt kEo Conglomerate K1G Reef limestone, limestone breccia N ( N ( N Kb-aC K K K sPZ2 Greenschist, phyllite, mudstone, chert vsNm Volcanic-sedimentary series vsT2 Volcanic-sedimentary series £ £ . . 8 8 partly marlstone (flysch) Boundary with lithological transition zone
( ( K K K Á Á Á Á
£ £ £ Proluvium - fanglomerate of rock fragments, 8 8 8 8 8 2 V V V (indefinite boundary) ( r Á Á Á Á
8 8 8 Limestone, partly marly and dolomitic DRIN - IVANICKI ELEMENT (D) Marble, recrystallised cherty limestone pQh lEo Valanginian - Hauterivian cPZ2 Á Á Á Á vpEo-Nm Pyroclastic rocks βT2 Meta-basalt
sandy-silty deposits V V V r o o Boundary of olistolith
8 8 8 8 Á Á Á Á r 8 8 Maastrichtian !( !( !( D D Î Î Î
2 Sandstone, marlstone, mudstone, partly ( o ( Conglomerate, sandstone, !( !( !( !( Quartzite, meta-sandstone, r
r Deluvium - rock fragments, sand, silt 8 8 sEo Kv-h D D D Rhyolite Î Î Granite, meta-granite
dQh N ( N ( N ( C !( !( !( qPZ2 πEo-Nm γT2 r tuffitic, magnesite and lignite bearing o o siltstone, partly limestone meta-conglomerate V s 8 8 DDD D D Î Î Î Axis of syncline
( N ( N ( kKmD Sandstone, conglomerate (flysch)
V DDDD V r Pleistocene Lower Oligocene N ( N ( N JURASSIC APZ2 Amphibolite, amphibole schist τEo-Nm Trachyte ST2 Serpentinite ø ø ( N ( N ( K K K K K D D D D r 8 8 8 Middle - Upper Jurassic ø ø sKmD Sandstone, siltstone, marlstone (flysch) Axis of anticline 0 0 ø ø Epidote schist, actinolite chlorite schist, 1 N ( N ( N K K K K K 0 0 cQp Calc tufa / travertine 8 8 lEo Reef (corals) limestone mPZ2 DDDD αEo-Nm Andesite PALAEOZOIC MAGMATIC EVENT s ø ø
0 < < < 0 o N Tectonic mélange with olistoliths - K K K K K partly muscovite schist, diabase 0 ( ( ( 8 8 8 < < < < KKK KKKKK D D D D D D D D 0 1 ( ( Coniacian - Maastrichtian J2-3 1 ( ( N ( o N 1 Conglomerate, sandstone, marlstone, sm limestone, schists, volcanic rocks K K K K Phyllites, sericite schist, quartz schist, r 6 ( ( Qp River terraces - gravel, sand kEo K< K< K< KKK fPZ2 D DDDD Eo-Nm Latite PZ Meta-porphyry, meta-keratophyre Overturned axis, syncline 6 4 t ( o N ( claystone, partly limestone, pyroclastic rocks o o λ D D D π Á 4 ( ( ( meta-sandstone D D D D D
8( 8 ( Limestone, marlstone, siltstone K K K Meta-sedimentary silicate rocks - K K K K
K K K
V V V o o o Kcn-mD K K K V r sJ2-3 8 8 8 (calcareous flysch) K K K K K K Biotite gneiss, biotite schist, V V V 8 8 CRETACEOUS o o schists, phyllites, gneisses K K K Basalt
lQp Lake sediments - gravel, sand, silt, clay K K K KKKKK K gPZ2 with marble intercalations βNp βPZ Meta-basalt s 8 8 8 V V V
( ( (
( K K K Overturned axis, anticline
Ø Ø Ø Ø
Ø Ø Ø Ø
Ø Ø Ø Ø Ø Ø Ø Ø K K K Ø Ø Ø Ø PASHTRIK CRETACEOUS (P) Î Î Î Î Á November 2006 Coniacian - Santonian cJ2-3 Meta-carbonate rocks - marbles, calcschists
ÎÎÎ ÎÎÎ
(
( 8 8
Ø Ø
Ø
Ø s
Ø Ø Ø
Ø Lower Palaeozoic Granodiorite Meta-granitic rocks
( (
Ø
Ø Qp Boulder field γδNm γPZ Ø
Ø Î ÎÎÎ Ø Ø b
Ø Ø Ø Ø Coniacian - Maastrichtian Orthometamorphic rocks - 8 8 8 Î Î Î
³ ³ ³ ³ ³ ³ ³ ³ ³ ³ 8 o 8 o Kcn-sD Reef and Rudist limestone AJ2-3 † Axis of fold Glacigene sediments - moraine, 8 8 amphibolite - metamorphic sole ³ ³ ³ ³ ³ ³ ³ ³ ³ ³ ³ ÎÎÎ gQp o 8 o 8 cPZ1 Marble JURASSIC MAGMATIC EVENT γδPZ Meta-granodiorite, meta-diorite ³ ³ ³ ³ ³ ³ ³ ³ ³ ³ Limestone, marlstone, calcarenite with chert fluvio- and limnoglacial deposits Kcn-mP Dip of axis syncline and of anticline 8 o 8 o Cenomanian - Turonian TRIASSIC !( !( !( !( Middle - Upper Jurassic Î Î Î Independent Commission for Mines and Minerals Beak Consultants GmbH NEOGENE o ( o o o o !( !( !( Quarzite, meta-conglomerate v v PZ Meta-syenite Turonian !( !( !( !( qPZ1 Î Î Î ζ Fault, observed ( o ( o o Olistoliths of cherty limestone v v v Am St. Niclas Schacht 13 Pliocene Kc-tD Conglomerate, breccia, sandstone, limestone lT J2-3 Volcanic-sedimentary series Komisioni i Pavarur për Miniera dhe Minerale o ( o o o o (uncertain age) v v vs V V V 8 8 APZ1 Amphibolite νPZ Meta-gabbro Fault, indicated 09599 Freiberg, Germany Upper Pliocene KtP Sandy limestone with Rudists V V V V V V 8 8 8 K K K K K Nezavisna Komisija za Rudnike i Minerale EXTERNAL VARDAR ZONE (E) Upper Triassic Epidote - chlorite - and actinolite schist, βJ2-3 Basalt Front of overthrust, observed Managing director: A. Barth ( 8 ( 2 Clastic sediments, clay, sand, gravel, K K K K K V V V ( Cenomanian o o K K K K K sPZ1 Á Á Á Á 8 8 Np Coniacian - Maastrichtian partly diabase, with marble intercalations Á Á Á Á Governing Board ( 8 ( partly marl, tuffite o o o o o olT3 Cherty limestone KKKKKKK KK ÁÁÁÁ vpJ2-3 Pyroclastic rocks Front of overthrust, indicated www.beak.de 8 8 o ( o ( o o Limestone, marlstone, siltstone o o K K K Phyllites Á Á Á Á Rr. Rrustem Statovci 29 Lower Pliocene KcP Conglomeratic banked limestone K KKK fPZ1 ÎÁ ! ÁÎ Á! ÎÁ o30 o ( o ( o o o fyKcn-mE (calcareous flysch) K K K Bedding, normal, dip of bedding ! Î ! Î ! o ( o Middle - Upper Triassic K KK KK KK γJ2-3 Granitic rocks Prishtinë, Kosovo K K K K Î Î Î h 8 8 8 1 Clastic sediments, clay, sand, gravel, 8 8 Biotite muscovite schist Î Î Î 45 o ( o Aptian - Cenomanian Marlstone, limestone K K K mPZ1 Foliation, normal, dip of foliation ! ! !
Np mKcn-mE 8 8 o ( o marl, carbonate lenses, burnt rock, lignite 8 8 8 KK KK K K Chairman: Naip Zeka N N Limestone, dolomite, partly cherty K K K ÎÎÎ Granodiorite 0 lT2-3 γδJ2-3 0 8 8 8 8 8 8 8 8 K K K
0 Sandstone, siltstone, KKK Biotite gneiss, leptinitic gneiss 0 V V V N N N gPZ1 V 0 Miocene 8 8 Ka-cP Thin-bedded limestone, calcarenite sKcn-mE 8 8 K K K www.kosovo-mining.org 0
0 N N conglomerate, marlstone, limestone K K K 0
8 8 8 Gabbro 0 0 V V V Lower - Middle Triassic K K K V νJ2-3 6 N ( o N ( Conglomerate, sandstone, . . NEOPROTEROZOIC 6 4 Aptian 4 ( Nm Kcn-mE Conglomerate V V o N o Meta-carbonate rocks - !( !( !( !(
marlstone, claystone . . .
!( !( !( σJ2-3 Peridotite, dunite, partly serpentinised Constructional area N o N ( N ( N cT1-2 marbles, calcareous schists K K K !( !( !( !( qNP Quarzite (cities, villages, etc.) Geology / Lithology Topography Scientific processing Upper Miocene N ( N ( N KaP Conglomerate, chert, sandstone Cenomanian !( !( !(
K K K Meta-sedimentary silicate rocks - V V N N N N N Pyroxenite, partly serpentinised K K K KKK sT1-2 schists, quartzite, meta-conglomerate ρJ2-3 Vector data based A. Knobloch, C. Legler N N 3 K K K K Amphibolite Main road Based on Osnovna Geološko Karta Nm Sandstone, marlstone, mudstone PAGARUSHA CRETACEOUS (G) KKK fKcE Phyllite, calcareous schist K K K ANP V V on Topographical maps N N N K K K K K K K K V V Serpentinite SFRJ 1 : 100,000 - Geološki Maastrichtian K K K Lower Triassic K K K SJ2-3 Regional road K K K K mNP Mainly mica schist, subordinately gneiss of former Yugoslavia 1 : 50,000 Cartography / GIS Middle - Upper Miocene ( N ( N CENTRAL VARDAR ZONE (C) K K K Institut, Beograd (1970-1984).
8 8 8 Railway KK KK K K o8 o N ( N ( N Sandstone, conglomerate (flysch) dT1 Limestone, dolomite K K K Mainly gneiss, subordinately mica edition 4-NIMA, series M709. 8 8 8 E. Dickmayer, A. Knobloch ( ( 2-3 sKmG Coniacian - Maastrichtian K K K 8 o 8 ( N ( N ( N ( N K KK gNP Nm Gravel, sand, clay, marl, marly limestone 8 8 8 8 8 K K K schist, leptite and granulitic rocks ( | | Water reservoir Reference system Copyright 1998 by the United o8 o N ( N ( N KK KK K
8 8 8 8 8 Conglomerate, sandstone, mudstone, breccia lKmG Rudist limestone Massive coralliferous limestone kT1 | | Mainly migmatitic rocks, partly granulitic, 8 8 bKcn-mC ( N ( N K K MNP States Government. No copyright Middle Miocene 8 8 8 8 8 subordinately different gneiss Ellipsoid: Bessel 1841 Map projection < < < K| K| River claimed under title 17 U.S.C. Santonian - Maastrichtian smKcn-mC Sedimentary mélange Datum: MGI Austria Transverse mercator 8 8 8 2 Marlstone, claystone, sandstone, < < < mNm o o o 8 o 8 Magnetic Declination 8 8 8 partly tuffstone and lignite < < < Limestone, marlstone, chert, calcarenite, N ( N ( N ooKs-m 8 o 8 o A B Line of cross section 8 8 8 2 G Thin-bedded limestone with chert < < < lKcn-mC partly conglomerate (calcareous flysch) 3.3° E ( N ( N kNm Gravel, sand, sandy clay, tuffs o o o 8 o 8 N ( N ( N Turonian Aptian - Cenomanian o N o 2 Sandstone, conglomerate, N o N sNm ( ( The information presented on this map has been collected from a variety of data sources. Although all data has been procured and researched with special diligence,
claystone, limestone, tuffs 8 8 0 Massive sandy limestone with Rudists ( ( ( Conglomerate, sandstone (flysch) it may be inherently inaccurate and imprecise. The user recognises that abstractions and adjustments are necessary for the map presentation of geoscientific data. 0 8 8 8 0 lKtG kKal-cC 0
0 Lower Miocene o ( o( 0 8 8
0 The publisher / author is not liable for any direct or indirect damages, losses, costs, charges or demands of any nature or kind resulting from incorrect / imprecise / 0 < < < Clastic sediments with diabase fragments - Marlstone, limestone, sandstone, 9 8 ( 8 o o 9 5 < < < sKtG mKal-cC incomplete data or incompetent use of data presented on this map. The user only is responsible for an appropriate use of all data presented on this map. The map is 5 ( 1 sedimentary mélange siltstone (flysch) 4 o o 4 8 8 Nm Conglomerate, sandstone, claystone < < < intended for use at the published scale only. Results of further detailed investigations may differ from data presented on this map. This map is not an authority on
( 8 8 international boundaries. 20°0'0"E 21°0'0"E
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