Download geological map of kosovo

GEOLOGICAL MAP OF KOSOVO
Scale 1 : 200,000
7420000
7430000
7440000
7450000
7460000
7470000
7480000
7490000
7500000
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4790000
4780000
4770000
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4730000
h
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h
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†
†
4700000
†
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†
†
h
h
4710000
o
†
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h
h
h
4690000
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†
45
†
o
nJ2-3
mPZ1
70
85
h
80
Triassic Metasandstone (Left Side) and Metadiabase (Right Side,
in the Foreground).
gdJ2-3
60
h
4670000
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GEOLOŠKA KARTA SR SRBIJE, 1 : 200,000 Beograd 1968, Zavod za Geološka i Geofizička Istraživanja, Languages:
Serbo-Croatian and French).
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o
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h
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GEOLOŠKI ATLAS SRBIJE (GEOLOGICAL ATLAS OF SERBIA), 1 : 2,000,000, published by Ministry for Mining and
Energetics Republic of Serbia and Geomagnetics Institute, ed. DIMITRIJEVIĆ M. D. et al., Beograd, 1994-2004, 16
map sheets themes
o
o
4630000
8
8
fPZ1
Phyllites
mPZ1
Biotite muscovite schist
(
!
(
!
(
!
K
K
K
K
(
!
!
(
(
!
K
K
K
K
K
K K KK
K
KK K
K
K K
K K
K
K K
K K
K
K
K
K K
K K
K
K
K
|K
|
K K K
K
K
|
K
|
K
|
K
|
Biotite gneiss, leptinitic gneiss
Î
Î
!
qNP
!
Î
!
Î
Quarzite
ANP
Amphibolite
mNP
Mainly mica schist, subordinately gneiss
gNP
Mainly gneiss, subordinately mica
schist, leptite and granulitic rocks
Mainly migmatitic rocks, partly granulitic,
subordinately different gneiss
MNP
!
Î
Î
Î Î
V
V
V
V
Latite
Volcanic-sedimentary series
bJ2-3
Basalt
vpJ2-3
Pyroclastic rocks
V
gdNm
V
Basalt
Granodiorite
V
bNp
D D D
V
lEo-Nm
D D D
Î
Î
Î
Î
Î
Î
Î
Î
Î
D D D D Á Á
Á
D D D
Á
gdJ2-3
Granodiorite
nJ2-3
Gabbro
sJ2-3
Peridotite, dunite, partly serpentinised
rJ2-3
Pyroxenite, partly serpentinised
SJ2-3
Serpentinite
4620000
- 1000
Granite, meta-granite
ST2
Serpentinite
Geological boundary, observed
Geological boundary, indicated
Boundary with lithological transition zone
(indefinite boundary)
Boundary of olistolith
s
r
r
s
Axis of syncline
Axis of anticline
Á
Á
r
Overturned axis, syncline
Meta-basalt
r
s
gPZ
Overturned axis, anticline
Meta-granitic rocks
s
pPZ
Meta-porphyry, meta-keratophyre
bPZ
†
November 2006
Axis of fold
gdPZ
Meta-granodiorite, meta-diorite
Î Î Î
Î Î Î
zPZ
Meta-syenite
Fault, observed
V
V
V
V
V
V
nPZ
Meta-gabbro
Fault, indicated
Independent Commission for Mines and Minerals
Komisioni i Pavarur për Miniera dhe Minerale
Nezavisna Komisija za Rudnike i Minerale
Dip of axis syncline and of anticline
Governing Board
Rr. Rrustem Statovci 29
Prishtinë, Kosovo
Chairman: Naip Zeka
www.kosovo-mining.org
Front of overthrust, indicated
Granitic rocks
0
D
Front of overthrust, observed
gJ2-3
1000
4610000
gT2
PALAEOZOIC MAGMATIC EVENT
Î
D
Á
D
Á
Á
Á
Á
Á
Á
Á
Á
Meta-basalt
Andesite
Î
Î
D
Á
D
Á
Á
Á
Á
Á
Á
Á
bT2
aEo-Nm
Î
Î
V
Á
Á
Á
Á
Á
Á
Á
Á
Î
Î
Î
(
!
(
!
(
!
!
V
(
!
(
!
(
!
!
!
NEOPROTEROZOIC
(
!
ÁV ÁV ÁV Á
Á Á Á Á
Á ÁÎ Á ÎÁ
Î
!
gPZ1
V
Volcanic-sedimentary series
Trachyte
V
Á
Á
Á
Á
Epidote - chlorite - and actinolite schist,
partly diabase, with marble intercalations
v
V
V
8
8 8
8
8 8
8
8
8
8
8
8
sPZ1
v
V
vsT2
Rhyolite
vsJ2-3
v
Á
Á
Á
Á
8
8
8
8
8
8
8 8
8
8 8
8
8
8
8
8
Amphibolite
v
Î
Á
D
Á
Á
m asl
gNP
Kv-hC
tEo-Nm
v
v
V
8 8
8
8 8
8
8 8
APZ1
v
V
Conglomerate, sandstone, mudstone, breccia
K
Quarzite, meta-conglomerate
Î
Î
Á
D
Á
Á
D
pEo-Nm
JURASSIC MAGMATIC EVENT
Middle - Upper Jurassic
V
kT1
K
qPZ1
Î
V
N
K
Marble
Î
Î
Î
V
(
(
N
K
Î
Î
Î
V
(
(N
N
K
Î
Î
V
(
N
Limestone, dolomite
K
(
!
K
dT1
Î
V
(N
!
(
K
K K
K K
KK K
K
K
K
K K
K K
K
K
K K
K K
K
K
K K
K K
K
K
Lower Triassic
N
(
!
(
!
V
sT1-2
(
!
(
!
!
(
D D D D D
V
< < <
< < < smKcn-mC Sedimentary mélange
o<8 <o <
8
8 o
<
< 8 <o lKcn-mC Limestone, marlstone, chert, calcarenite,
partly conglomerate (calcareous flysch)
o8 o8
cT1-2
gPZ2
D D D D D
V
bKcn-mC Massive coralliferous limestone
K K K
K K K
K K K
K K K
Meta-carbonate rocks marbles, calcareous schists
Meta-sedimentary silicate rocks schists, quartzite, meta-conglomerate
fPZ2
D D D D
D D D D D
V
Cenomanian
K K K
K K K K
K K K
Phyllite, calcareous schist
K K K K fKcE
K K K
CENTRAL VARDAR ZONE (C)
Coniacian - Maastrichtian
Lower - Middle Triassic
D D D D
Á
Á
Á
K K
K K
K K
K K
K K
K
V
Conglomerate
K
Limestone, dolomite, partly cherty
Epidote schist, actinolite chlorite schist,
partly muscovite schist, diabase
Phyllites, sericite schist, quartz schist,
meta-sandstone
Biotite gneiss, biotite schist,
with marble intercalations
D
D
D
DDD D D
Î
V
Kcn-mE
Middle - Upper Triassic
lT2-3
(
!
(
!
KKKKK
KKKKK
KKKKK
K
KK
K KKKK
K
K K K
K K K K
K K K
K KK KK KK
Cherty limestone
mPZ2
cPZ1
(
!
(
!
Olistoliths of cherty limestone
(uncertain age)
D D D D
Lower Palaeozoic
(
!
Upper Triassic
o o
o o o lT3
o o
K K
K
K
K K
K
K
Amphibolite, amphibole schist
Pyroclastic rocks
V
AJ2-3
Orthometamorphic rocks amphibolite - metamorphic sole
K
K
v
K
K
APZ2
vpEo-Nm
vpEo-Nm aEo-Nm
Kb-aC
30
Bedding, normal, dip of bedding
45
Foliation, normal, dip of foliation
Constructional area
(cities, villages, etc.)
Geology / Lithology
Based on Osnovna Geološko Karta
SFRJ 1 : 100,000 - Geološki
Institut, Beograd (1970-1984).
Main road
Regional road
Railway
Reference system
Ellipsoid: Bessel 1841
Datum: MGI Austria
Water reservoir
River
A
B
Line of cross section
Beak Consultants GmbH
Am St. Niclas Schacht 13
09599 Freiberg, Germany
Managing director: A. Barth
www.beak.de
4600000
h
o
Thin-bedded limestone with chert
Meta-carbonate rocks - marbles, calcschists
qPZ2
Quartzite, meta-sandstone,
meta-conglomerate
mKcn-mE
Lumi i Badlavës
mKal-cC
Topography
Vector data based
on Topographical maps
of former Yugoslavia 1 : 50,000
edition 4-NIMA, series M709.
Copyright 1998 by the United
States Government. No copyright
claimed under title 17 U.S.C.
Magnetic Declination
3.3° E
Scientific processing
A. Knobloch, C. Legler
Cartography / GIS
E. Dickmayer, A. Knobloch
Map projection
Transverse mercator
Aptian - Cenomanian
< < <
< < < sKtG
< < <
lKtG
Massive sandy limestone with Rudists
Clastic sediments with diabase fragments sedimentary mélange
(
(
o ( o(
o o
o o
(
(
(
kKal-cC
Conglomerate, sandstone (flysch)
mKal-cC
Marlstone, limestone, sandstone,
siltstone (flysch)
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,
it may be inherently inaccurate and imprecise. The user recognises that abstractions and adjustments are necessary for the map presentation of geoscientific data.
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 /
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
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
international boundaries.
21°0'0"E
7440000
7450000
7460000
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7490000
7500000
7510000
7520000
7530000
7540000
7550000
7560000
4590000
o
o
Rudist limestone
.
cJ2-3
Marble, recrystallised cherty limestone
dQh
B
NE
Majdan / Braine Cenozoic
volcanic complex
Á
Á
o
o
lKmG
.
sJ2-3
KKKKK
KKKKK
KKKKK
KK
KK
K KKK
K K K K
K K K
KK KKK KK
KKK K
K
K
K K
K
v
N
.
sKcn-mE
Sandstone, siltstone,
conglomerate, marlstone, limestone
(
!
v
N
N
mKcn-mE Marlstone, limestone
(
!
!
(
Á Á Á Á
Á DÁ Á
Á
D
cPZ2
Internal Vardar subzone
Á
Á
Á
Á
o
Sandstone, conglomerate (flysch)
Limestone, marlstone, siltstone
N
N
(
!
(
!
Tectonic mélange with olistoliths limestone, schists, volcanic rocks
Meta-sedimentary silicate rocks schists, phyllites, gneisses
< < <
< < < < J2-3
sm
K< K< K<
o o o
o o
Conglomerate, breccia, sandstone, limestone
o o o lT
fyKcn-mE (calcareous flysch)
(
!
(
!
v
N
N
(
!
JURASSIC
Middle - Upper Jurassic
K K K
K K K
K K K
(
!
v
o Kv-hC
(
Conglomerate, sandstone,
siltstone, partly limestone
TRIASSIC
EXTERNAL VARDAR ZONE (E)
Coniacian - Maastrichtian
o o
o o
4640000
o
Conglomerate, chert, sandstone
Kc-tD
o
4660000
The gradual development of Cenozoic sedimentation basins ranging from the Eocene basin in the NE (outside
Kosovo) to the Pliocene basin in the SW was accompanied by intensive post-collisional andesitic volcanism inside
the Vardar zone. The volcanic activity in the Kosovo area, which started in the Oligocene and had its main phase
during Miocene, also brought up granodioritic masses. The sedimentary basins are masked on the pre-Neogene
structures trending preferentially in NW-SE and NE-SW direction. Their activity continued until the Quaternary.
mPZ1
4650000
h
o
(
4680000
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o
h
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42°0'0"N
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Reef and Rudist limestone
o
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Turonian
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o
o
o
h
Conglomeratic banked limestone
Santonian - Maastrichtian
7430000
h
h
h
h
h
h
h
h
h
h
h
o
o
h
8
h
h
h
†
h
h
h
h
o
h
o
o
o
h
h
o
(
(
!
20°0'0"E
7420000
h
h
h
h
h
h
h
h
h
h
h
o
h
h
o
o o
h
o
h
8
h
h
h h
h
h
h
†
h
h
h
h
h
h hh
s
r
o
o
h
h
h
h
o
o
h
42
57
gPZ58
12
60
qPZ1 o
DARDANIA MASSIF
oh
8
h
r
h
h
h
o
h
h
s
o25
v
o
Volcanic-sedimentary series
V
o
vsNm
V
Valanginian - Hauterivian
Greenschist, phyllite, mudstone, chert
V
o
o
(
Sandstone, siltstone, conglomerate,
partly marlstone (flysch)
V
r
†
h
h
Á
r
h
s
†
o
o
h
h
h
o
SJ2-3
25
TRIASSIC MAGMATIC EVENT
Middle Triassic
V
Sandy limestone with Rudists
Kcn-sD
Cenomanian - Turonian
Kb-aC
CENOZOIC MAGMATIC EVENT
Oligocene - Pliocene
V
r
†
o
o
o
o
h
o
o
o
20
sJ2-3
v
N
PALAEOZOIC
Upper Palaeozoic
K K K
K K K
K K K sPZ2
K K K
smKcn-mC
v
(
sJ2-3
SJ2-3
Ks-mG
v
Limestone, marlstone, siltstone
(calcareous flysch)
N
Coniacian - Santonian
o
lKtG
v
Kcn-mD
(N
(
v
v
sKtG
pQh
tQp
v
Sandstone, siltstone, marlstone (flysch)
(N
N
aQh
v
³
³
³
³
³
³
†
h
o
o
o
o
o
o
o
o o
o
o o
o o o
o
o
o
o
o
o o
o
o o
o
o
o
o o
o
o
o
o
o
h
h
o65
smKcn-mC
Lumi i Sitnicës
v
³
³
³
³
³
h
h
o
o
o
o
o
60
62
79
sPZ1
44
During the Neogene, fracturing and subsidence of intramontane basins became most important. On one side, the
southwestern areas (Albania) have been influenced by marine ingression during the Oligocene and Miocene. On
the other side, the area of today’s Kosovo was dominated by silty-clayey lacustrine-terrestrial sedimentation (with
important lignite deposits) mainly during the Miocene and Pliocene.
Vardar Lower Cretaceous Flysch trough
v V
v
v
v
sKmD
vV
v
v
cT1-2
sT1-2
K
K K K
K K K
K K
K K K K K K K K K K
K K K K K K K K K K K K
v
V
v
sKmD
v
Sandstone, conglomerate (flysch)
smJ2-3
tQp
v
o o
o o
o o
Kcn-sD
v
(
(N
sKmD
v
³
³
³
³
³
³
o
o
o
o
o
o
o
o
o
85
OSNOVNA GEOLOŠKA KARTA SFRJ, 1 : 100,000, Beograd/Titograd/Skopje1970-1984, Geozavod Beograd/Geološki
Institut Beograd, Zavod za geološka istraživanja SR Crna Gora, Geološki zavod Skopje, Language: SerboCroatian).
15
Kosovo Cenozoic basin
Np1
V
8
!
o
o
o
o
o
s
s
h
o75
Central Vardar subzone
v
kKmD
N
N
lQp
vsT2
V
8
!
o
o
o
o
o
65
60
65
56
30
mPZ1
Nm3
Rahovec Ophiolite Complex (Basalt Pillows and Plagio-Rhyolite).
10
v
(
(N
Np
Np1
v
8
!
o
o
43°0'0"N
!
o
o
o
o
o
o
s
Á
s
h
5
Çiçavica Triassic unit
v
N
(
(
Denac
1
v
v
Drenicë Cenozoic basin
Carralevë
Upper Cretaceous unit
V
8
IF
GO
o
o
o
o
o
h
h
h
h
42°0'0"N
SS
4760000
MA
IF
LA
4750000
AN
CH
SS
PE
o
o
4740000
NI
AN
MA
UB
E
o
o
o
h
4730000
DO
BR
NE
IT E
ZO
OL
AN
Z ON
o
h
4720000
CE
AR
HI
NI
VO
RO
o
o
h
4710000
MA
RD
OP
GO
AV
(S
NE
-G
s
r
o
o
o
h
4700000
O-
N
ZO
A
o
o
4690000
!
RB
ER
VA
ST
LI
UJ
o
o
h
4680000
!
SE
EA
KA
o
o
o
h
h
h
4670000
C
!!
LA
NE
ZO
CH
ÇU
KR
NE
o
h
h
h
h
4660000
!
PE
BI
RA
A-
AN
HT
BR
AS
IT E
KO
IO L
KR
ZO
o
o
o
o
h
h
h
4650000
!
PH
AN
S
o
o
h
h
h
h
h
h
4640000
AR
AO
NI
o
o
o
h
o
h
h
h
4630000
ES
N
!
DIT
IO
o
o
o
I DE
o
EN
o
o
o
o
h
h
o
h
o45
VARDAR ZONE
V
4620000
!
TID
!
!
MIR
LL
o
o
o
o
h
h
57
gPZh
35
1 : 200,000
V
4610000
A IŠ
KA
!
!
A
o
HE
o o
o
o
o
h
h
o
30
vV
4600000
KR
NT
NI
o
o
o
o
h
h
h
APZ1
37
50
qNP
SJ2-3
AJ2-3
45
V
4590000
GETICU
M
ME
VI
S
o
o
o
h
h
h
h
20
70
E
EL
ER
o
o
ID E
o
o
AR
o
o
o
h
h
h
o
o20
SJ2-3
sJ2-3
sNm
72
55
50
45
25
cPZ1
37
2
gPZ
o40
gdPZ
v
Conglomerate, sandstone, claystone
55
qNP
70
78
gNP
35
30
GEOLOŠKO-TEKTONSKA KARTA SAP KOSOVO, 1 : 100,000, Zagreb 1974, Geozavod Zagreb, Language: SerboCroatian.
v
(
dQh
sPZ1
h65
20
ANP43
GEOLOGICAL MAP OF YUGOSLAVIA, 1 : 500,000 (printed 1971, 6 map sheets).
v
Sandstone, conglomerate,
claystone, limestone, tuffs
o65
o
20
V
sNm2
(
(N
N
Coniacian - Maastrichtian
sKmG
o o
o o Ks-mG
o o
-H
o
o
h
h
h
20
V
(N
D IN
o
o
o
h
h h
qPZ2
dQh
h
50
o45
50
30
h
15
V
N
h30
cPZ1
SJ2-3
h35
Folded Upper Cretaceous Platy Limestone (Carbonate Platform).
V
(
o75
lT2-3
60
APZ1
h
65
30
40
o44 Kcn-mE
25
V
(N
(N
h40 nJ2-3
lT2-3
20
V
Gravel, sand, sandy clay, tuffs
KaP
A TIA N
o
o o
o
h
gQp
KI
LM
o o
o
o
o
o o o
o
h
30
gdPZ
IC
DA
o
o
o
o
o
o
o
o
h
o40
o40
cPZ1
nPZ
V
N
Reef limestone, limestone breccia
Conglomerate, sandstone, marlstone,
claystone, partly limestone, pyroclastic rocks
N
N
(
N
.
(
fyKcn-mE
h
55
60
h
cPZ1
MNP
cPZ1
gPZ
80
MNP
Selected Literature and Sources of Data
V
(
(N
N
.
(N
N
h55 o65
gPZ
The map has been compiled in ArcMap GIS format. It is a feature of the GEO-Database Kosovo, in which more
information is stored providing the possibility of combining various thematic information. For detailed information
see www.kosovo-mining.org. Available documentation and used literature can be acquired via ICMM.
V
kNm2
Ka-cP
o50
40
30
h
mPZ1
tQp
The geological formations have been delineated based on the information shown on older geological maps. The
recent map features a unified legend of the geological formations, which was applied all over Kosovo. The legend
comprises a stratigraphic classification of the formation (fill colour), as well as of a representation of the rock
lithology / genesis / petrography / alteration (fill pattern). The classification of the geological formation concerning
stratigraphy and lithology can also be derived from the rock abbreviation used on the map. Beside this, the map
contains information about the main geological boundaries and the most important tectonic elements.
V
mNm
8
8 Nm1
( 8
(
(
40
h
o
MNP
65
25
h
60
gPZ1
60
o45 h
o
80
o65
o50
o
Gravel, sand, clay, marl, marly limestone
Marlstone, claystone, sandstone,
partly tuffstone and lignite
2
(N
N
Lower Miocene
(
(
o
o KcP
K1G
N
PAGARUSHA CRETACEOUS (G)
Maastrichtian
Sandstone, marlstone, mudstone
8Middle8Miocene
N
(
N
Nm3
o
h
60
25
o
qPZ1
h
25
h50
o30
o
80
50
o60
h30
h
(N
N
o8 o
8 ( o 8 ( Nm2-3
o8 ( o
(
(
h70
qPZ1
h60
50
35
50
gPZ
lEo2
aQh
smKcn-mC
lEo1
36
30
mNm2
30
vpEo-Nm 50
o50
o80
h50
Kcn-mE
25
MACEDONIA
h
20
36
Barremian - Aptian
Reef (corals) limestone
Aptian
Middle - Upper Miocene
8
8
8
(
o
cPZ1
30
dQh
gQp
o50
o65
20
s
r
Conglomerate, sandstone,
marlstone, claystone
o
N
o
(
Aptian - Cenomanian
Upper Miocene
N
lT2-3
40
40
o70
kEo
o60 lEo
h
o N(
o N ( o Nm
N
oN
(
bQp
40
fyKcn-mE
o75
h60
cPZ1
1
1
h
o
Clastic sediments, clay, sand, gravel,
marl, carbonate lenses, burnt rock, lignite
N(
o
sPZ1
60
o75
50
58
65
60
lKcn-mC
cPZ1
gNP
sNm2
12
70
35
lEo1
56
mNm2
dQh
65
85
o
mNm2
gPZ
10
mNm2
nJ2-3
vpEo-Nm
28
aQh
48
pQh
h
o
o
N
(
KtP
h60
52
mNm2
55
lQp
MNP
sEo2
60
tEo-Nm
pQh
15
fPZ2
h
20
50
50
70
mNm2
25
14 mPZ2
h
30
10
o
30
bPZ
35
†
30
20
o
v
DRIN - IVANICKI ELEMENT (D)
Maastrichtian
N
Cenomanian
o
Miocene
N
Np
65
30
50
mNm2
o
nJ2-3
SJ2-3
bJ2-3
1
50
h30
60
nJ2-3
o
cPZ2
30
47
†
o
o o
o
30
o
Clastic sediments, clay, sand, gravel,
partly marl, tuffite
o ( o
8 8 Np1
o8
o( o
( o
o
Sandstone, marlstone, mudstone, partly
tuffitic, magnesite and lignite bearing
Turonian
Lower Pliocene
N
Limestone, partly marly and dolomitic
8 o 8 o
o 8 o 8 Kcn-mP Limestone, marlstone, calcarenite with chert
8 o 8 o
Glacigene sediments - moraine,
fluvio- and limnoglacial deposits
gQp
8(
(
8 ( 8 Np2
8(
(
8
8
N
o
h
50
o
o
Boulder field
NEOGENE
Pliocene
Upper Pliocene
N
h50
60
80
40
15
85
aQh
60
30
57
o
nJ2-3
vpEo-Nm
46
36
kNm2
65
gQp
19
h
mPZ2
qPZ2
32
20
o
bQp
(N
Conglomerate
CRETACEOUS
PASHTRIK CRETACEOUS (P)
Coniacian - Maastrichtian
Lake sediments - gravel, sand, silt, clay
50
60
kEo1
50
v
V
River terraces - gravel, sand
Np1
50
70
10
32
30
8
Gjilan/Gnjilane
80
gPZ
h56
68
fPZ1
o
o
v
V
ø ø
ø ø
ø ø
ø ø
tQp
( 8 ( 8(
8 ( 8 8(
8 8
8 8 8 lQp
lEo1
oN
N( o N
1
o N ( kEo
(
o
Calc tufa / travertine
70
20
24
gQp
bPZ
fPZ2
Ks-mG
lKtG
tQp
Np
V
V
V
Mirushë
1
Lower Cretaceous
Lower Oligocene
cQp
h30
75
cPZ2
V
V
V
V
V
V
V
V
V
V
V
V
V
V
V
V
V
V
V
V
V
V
K1G
dQh
V
Deluvium - rock fragments, sand, silt
45
70
80
h
gdPZ
20
s
sJ2-3
V
lEo2
8 8
8 8 sEo2
8 8
Pleistocene
N
kEo2
80
50
sPZ1
o25
49
Mirushë Cenozoic basin
Pagarushë Upper
Cretaceous anticline
V
V
dQh
.
.
h80
40
60
80
65
h45
53
38
THE COMPILATION OF THE GEOSCIENTIFIC MAPS OF KOSOVO – GEOLOGICAL MAP 1 : 100,000 – Description of the Map
Compilation – Beak Consultants GmbH, Prishtinë, March 2006, 175 p.
bJ2-3
V
V
V
V
V
V
V
V
V
V
Proluvium - fanglomerate of rock fragments,
sandy-silty deposits
pQh
.
.
smJ2-3
70
60
Kilometres
aQh
sJ2-3
V
V
V
.
Alluvium - gravel, sand, silt
70
80
65
gPZ50
60
60
lQp
fPZ1
0
Drini i Bardhë
aQh
V
V
V
V
V
V
V
V
£( £( £
£( £(
aQh
£
£ (
£
(
70
70
20
35
cPZ1
gNP
42
45
50
72
65
In the Pleistocene, the highest mountains were covered by glaciers. Their glacigene (moraines, lacustrine and
fluvial) deposits occur in southern and western part of Kosovo. River terrace sediments can be found up to
hundred metres above the actual stream level. Deluvial debris, proluvial fanglomerates and alluvial sandy-gravely
deposits in the youngest valleys are of Holocene age.
30
20
40
fPZ2
Rahovec Jurassic
Ophiolite complex
PALAEOGENE
Oligocene
Upper Oligocene
QUATERNARY
Holocene
h50
70
25
r
h45
V
V
V
V
V
V
V
Legend
(
Np1
40
60
h
50
70
gNP
34
50
38
56
MNP
38
30
h
gJ2-3
mKal-cC
45
80
28
h
25
vsJ2-3
(N
h50
70
gQp
h25
lT2-3
30
80
60
70
75
50
60
o80
80
Np1
gPZ
DRIN - IVANICKI ELEMENT
Proni i Beces
V
V
V
V
V
0
N
15
h
80
60
42
35
48
40
48
15
60
dQh
70
30
- 1000
(
70
50
50
20
50
65
80
30
smJ2-3
70
45
fPZ2
20
o
KaP
1000
N
50
20
40
25
80
70
34
50
ANP
28
54
70
46
38
MNP
44
35
15
65
nJ2-3
65
35
20
48
60
cJ2-3
nJ2-3
50
80
35
h25
15
25
43
gNP
30
lEo2
65
MNP
38
40
48
aEo-Nm
80
h45
34
35
sPZ1 50
50
70
sJ2-3
57
40
65
65
30
40
55
37
†
40
20
43
32
42
mNP
42
30
ANP
0
30
60
80
75
40
The youngest tectonic activity generated vertical movements, uplifting and subsiding of separated blocks. The
central depression (Pejë / Peć – Prizren / Prizren) is a downthrown block (the total subsiding exceeds more than
thousand metres), surrounded by upthrown blocks, which still ascend with an uplift rate of 0.4 mm per year.
35
h
zPZ
20
pEo-Nm
h
sJ2-3
tQp
Np2
50
55
25
44
60
32
50
30
h41
Scale 1 : 200,000
Dukagjin basin
Gjakovë Cenozoic subbasin
Erenik
80
gPZ
70
gJ2-3
bJ2-3
70
65
50
10
h24
SW
N
h80
h70
15
aQh
Kcn-mD
External Vardar subzone
Np2
70
80
40
60
58
30
47
40
25
30
h
76
30
70
60
30
33
h
40
gNP
h45
38
APZ1 vpEo-Nm
50
85
65
o70 tEo-Nm
smJ2-3
h50
60
80
70
35
80
60
70
h46
80
80
40
24
h
qPZ1
40
h
50
OPHIOLITE BELT
m asl
h85
20
The low-grade metamorphic rocks, which are common in the Kosovo territory, have to be interpreted in the frame
of the extensive subduction processes. In general, the exposure of these rocks has to be connected to the
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
tectonically and palaeographically uncertain position.
N
h
h
pPZ
25
30
N
h
qPZ2 h
45
45
pPZ
The SW-vergent structures of the Dinarides were formed by geodynamic overthrusting of the geotectonic units
from NE to SW in the Palaeogene age. As a result, the Triassic East Bosnian-Durmitor zone is lying above the
Adrian foredeep and the Dardania massif / Serbo-Macedonian massif pushed the Vardar zone against the
Palaeozoic-Triassic Drin-Ivanicki Element. The Peri-Adriatic Fault (PAF) is seen as the lateral shear lineament
between the accreted structural elements (terranes).
N
h
40
30
Both, the appearance of the microplates together with the accretion of partly small terranes and the transition to
younger folding towards SW are characteristic features for the Balkan Peninsula. By the end of the Upper
Cretaceous, in the Palaeogene, the subduction was followed by a continent-continent-collision, which led to
strong collisional deformation, the uplift of the Dinarides blocks and the overthrusting of flat nappes toward SW.
This phase was accompanied by granite plutonism and andesite volcanism in some parts of the Balkan Peninsula
and metamorphism of some parts of the Mesozoic graben-sediments. The cumulative tectonic shortening of the
crust has been estimated with 500 km.
N
o
h
pPZ
60
Compressional tectonics due to subduction-collision mechanisms transformed the basins and platforms into fold
and thrust zones in the late stage of the orogenic deformation. As a result of the stable tectonic setting, all major
Mesozoic palaeographical units turned into fold and thrust zones, starting NE to SW.
Gjakovë Jurassic
peridotite complex
80
o
80
cPZ1
60
70
86
qPZ1
40
zPZ
75
pQh
1 APZ2
Np45
50
o
60 80
E)
30
38
20
50
nJ2-3
60
30
N
h
h
h
h45
70
35
78
SJ2-3
45
40
60
kKal-cC
12
75
h
30
7
30
30
h
gQp
30
Np
42
lEo
40
60
40
1
70
h
lQp
35
h
h
h45
15
h
55
h
gPZ
nPZ
55
o30
20
30
h
30
sPZ1
h35
40
h
bJ2-3
60
65
h40
Kcn-mE35
30
10
26
qPZ1
h30
pPZ
fPZ1
sPZ1
h75
h35
lT2-3
35
h
h
o
o
fPZ2
35
aQh
gQp
15
30
35
h
lQp
h40
h
p
55
h55
20
h30
h80
70
70
sQp
45
40
75
60
50
lT2-3
lT
50
45
80
32
80
qPZ1
53
2
60
h
80
60
80
40
50
80
75
h50
h45
35
60
60
o30
Ferizaj/Uroševac
h80
60
h
sJ2-3
27
dQh
h80
40
lQp
15
h70
h60
h30
sJ2-3
sJ2-3
60
80
18
mKal-cC
80
60 50
76
80 87
80
gPZ70
50
†
40
50
80
58
75
mNP
28
sEo2
2
kEo
70
50
sPZ1
gQp
70
lKcn-mC
70
80
sJ2-3
50
o82
30
o60
40
s
r
h25
AJ2-3
70
sm82Kcn-mC
32
h42
70
35
75
h
25
80
65
50
o22
kKal-cC
40
APZ1
o85
70
25
42
cJ2-3
75
85
15
45
50
80
o40
25
o
30
h
60
60
h30
o
h
30
50
Qh h45
40
o38
h
30
h
fPZ2 h25
h
o
o
o
h
h
h
h
h
45
80
40
45
h
AJ2-3
15
h
43
35
40
The subduction of an oceanic plate underneath the continental crust of the Carpatho-Balkan arc started in Lower
Cretaceous. Hence, the Vardar zone ophiolites may be obducted during this process, whereas the Kopaonik
block can be interpreted as the island arc, which was separated from the Rhodopes and Dardania massif / SerboMacedonian massif by this marginal basin. These ophiolites were partly accreted onto the active continental
margin and covered by rudist limestones and flysch sediments in the Upper Cretaceous. The formation of flysch
sediments in the Vardar zone is proven since higher Lower Cretaceous. In some areas (only outside of Kosovo)
basal parts of flysch are interlayered with basalts and rhyolites and intruded by anorogenic intraplates granites.
Olistostrome horizons are very common in Upper Cretaceous.
h
h
h
o
30
30
o
28
40
lT2-3
25
gQp
28
o50
25
40
h
h
15
45
o
h45
35
dQh
35
s
40
h
82
70
30
80
70
h
30
bJ2-3
80
70
30
o25
65
cJ2-3
70
20
40
h
80
h80
smJ2-3
50
70
30
lT2-3
25
35
h
10
40
70
cT1-2
mPZ2
lT
30
o35
40
r
25
h
SJ2-3 cPZ1
45
60
mKal-cC
50
h70
40
Z ON
17
15
40
mKal-cC
60
26
35
80
60
Kv-hC
65
sT1-2
h50
50
70
40
h45
25
60
40
40
40
h
dQh
70
lT2-3
h35
SJ2-3
o
75
50
80
75
50
o45
35
AJ2-3
35
70
40
60
60
h40
50
60
sT1-2
Kcn-mD APZ2
o40
o40
h80
o80
30
20
50
h
22
20
40
45
sPZ1
60
40
o
50
60
h
o
o
15
o
70
35
pQh
65
60
h20
85
lT2-3
70
40
40
h
o
h
h
tQp
50
60
80
40
AN
70
40
65
35
42
70
65
Np
70
83
63
40
80
1
70
32
80
fPZ2
80
M AS SIF
Aegean Sea
NI
vpEo-Nm
sEo2
kKal-cC
65
25
25
60
40
70
80
50
85
40
80
70
SJ2-3
aQh
85
45
h
50
lT
60
45
h
o
smJ2-3
15
40
40
26
25
lT2-3
35
70
70
20
60
sJ2-3
50
h
20
20
25
70
Np2
30
20
25
o
25
80
62
h45
45
h
h
50
80
h h60
smJ2-3
h
o
o
h
h
o
20
50
87
pQh
60
sKmD
40 45
o
60
h
dQh
15
70
30
80
o25 Kc-tD
o70
h25
30
h30
20
o
42
70
35
h70
50
h
40
76
bJ2-3
60
70
50
R HO D OPE
gNP
65
40
70
60
50
45
80
27
h
o
o
Prizren/Prizren
55
lT h
o80
75
60
50
h40
45
25
40
62
s
s
40
45
h
o
o
o
KtP o
58
67
h
65
h
45
lQp
25
o15
The Vardar zone (Vardar ocean) and parts of the Dinarides Zone (Mirdita respectively Budva-Pindos oceanic
basin) are regarded as an oceanic crust area, divided by the Pelagonian platform. The Middle to Upper Jurassic
ophiolites comprise a thick sequence of ultramafic, basic as well as basaltic rocks, which possibly syn-kinetically
(in connection with the sea floor formation), but mainly post-kinetically (in connection with later tectonic
transportational processes) have been serpentinised, mostly. At the end of the Upper Jurassic and the Lowest
Cretaceous, the ocean was closed again. Early Cretaceous “pre-flysch” is composed of fossiliferous clastic rocks,
which are unconformable overlain by Upper Cretaceous carbonate followed by mainly sandy-silty flysch
sequences.
N
h
h
o
o
o
25
17
pQh
50
o25
20
o17
AJ2-3
o
50
A separate barrier with Upper Palaeozoic rocks exists between the Vardar zone in the NE and the Inner-Dinarides
in the SW since the Triassic. The flanks of this barrier have been dominated by extensive gravitational marine
sediment transports directed towards the Inner-Dinarides trough. Later on, after folding and sliding movements,
this barrier probably formed the Drin-Ivanicki element.
( (
h
r
30
o
o
o
s
10
15
15
o35
o
o
KcP
25
o
20
15
o
15
20
r
40
lT2-3
Np2
15
†
36
40
70
50
Á
Á
fPZ2
67
o50 70
75
75
Tirana
NIDES
35
35
80
70
70 70
70
70
70
70
r
53
70
70
aEo-Nm
30
h70
42
70
35
60
84
70
68
45
o50
35
!
(
E
SR ED NA G
O RA
B A LK A
High-Grade Metamorphic Rocks (Migmatitic Gneiss) in the Kaçanik
Metamorphic Unit.
85
40
sT1-2
mPZ2
45
h
o
o
o
25
25
o
o15
20
25
Kcn-mP o
23
h
30
h
Np2
35
sJ2-3
pQh
70
o
50
65
80
30
45
70
!
(
Skopje
55
45
35
60
SJ2-3
h70 60
h
82
cT1-2
cPZ2
cPZ2
80
h
h25
h
28
60
35
70
55
30
56
60
55
smKcn-mC
20
o
gPZ2
66
h
vsJ2-3
h25
35
60
40
SJ2-3
45
Np1
80
N
!
(
aEo-Nm
70
50
60
50
60
pQh
60
!
Kcn-mD
22
55
70
60
o
o
o
20
50
25
h
o o
o
35
The Inner-Dinarides trough, which is located southwest of the Vardar zone, also got subdivided into barriers and
basins since the Triassic, so facies differences have to be looked at in detail. The occurrences of volcanicsedimentary series starting in Middle Triassic age are a common feature. Basic and ultra-basic magmatic
activities have probably been connected to the creation of deep fault zones (rifting) and the formation of the first
oceanic crust (opening of the parts of Tethys ocean).
(
( (
40
o18
40
85
Kcn-sD
47
30
h
sJ2-3
85
70
35
h
pQh
lQp
65
sPZ1
70
h60
40
35
40
h
o
o
o25
o25
28
35
18
35
25
o
o
pQh
o
o
o
20
35
KtP
o25
25
The Vardar zone represents the most mobile zone of the Dinarides-Hellenides. This lithologically heterogeneous
and tectonically complicated zone was built in the Upper Jurassic and Lower Cretaceous after the stable
Palaeozoic crust broke apart and a system of troughs and barriers was generated. In this area, shallow marine
limestone can be found up to the Upper Triassic (marine carbonate platform). The separated Dardania massif /
Serbo-Macedonian massif became a mainland, thus dominated by erosion. Other areas of stable continental crust
already started to break up during the Middle Triassic age, which led to the formation of small troughs,
accompanied by more or less intensive rift volcanism.
A
35
20
Np2
lQp
h50
64
30
o
h
Np2
o
o
o
Ka-cP
Kosovo is characterised by a variety of geological formations ranging from old crystalline Proterozoic to youngest
Quaternary age, comprising sedimentary and magmatic rocks together with rather less frequent metamorphic
rocks.
Schematic Geological Cross Section across Kosovo
†
55
50
80
cT1-2
Á
Kv-hC
50
25
o65
42
smJ2-3
80
60
70
h
o35
Prishtinë/Priština
40
57
48
80
80
Prishtinë
FORE BALKAN
STARA PLANINA ZONE
Sofia
!
B
30
20
80
50
h
o70
35
h50
80
gPZ
†
32
45
50
25
30
46
85
o
o
o
o o
o
Np2
22
45
30
fPZ2
h
o
o
32
h
h
o
o
o
15
25
o
o
25
o
h
h
o
o
o
30
45
60
o
8
aQh
h
o
h
h
h
h
o
o
o
o
22
o
lQp
The oldest core of the Balkan Peninsula is situated within the Circum Rhodope belt with medium- to high-grademetamorphic crystalline units (Dardania massif / Serbo-Macedonian massif, Rhodope massif, Geticum etc.) and
the marginal zones of the Pelagonian massif. As a result of Palaeozoic subduction and Hercynian collision, these
Proterozoic and Palaeozoic continental massifs have been merged into a single continent. The Triassic
intracontinental rifting led to the break-up of the Palaeozoic continent and to a different evolution of the
microcontinents. Later, parts of it (e.g. the Dardania massif / Serbo-Macedonian massif) were tectonically
separated and structurally incorporated into the Alpine evolution.
o
h
o o
o
35
sJ2-3
38
70
s
45
!
sEo2
35
50
55
o
o
o
30
20
20
48
45
lKcn-mC
pQh
60
cPZ2 qPZ2
30
o35
lQp
o
25
h
o
o
o
o
o
o
18
12
Np
nJ2-3
o
o
o
o
o
o
o
10
h
o
32
33
o
o o
39
35
30
o
60
2
o20
rJ2-3
h
50
54
65
!
!
vpEo-Nm
80
56
52
80
65
o50
56
28
18
MOESIAN PLATFORM
smJ2-3
85
75
bKcn-mC
45
Kb-aC
72
30
35
!
(
Bucureşti
30
70
Kv-hC
o60
smKcn-mC
68
dQh
Np
60
CARPATHIANS FOREDEEP
75
44
70
55
76
h
gPZ2
40
Kcn-mP
rJ2-3
SJ2-3
o
o
o
s
r
o
20
60
sKmD
o
10
o
o
65
12
o
40
28
35
h60
!
E
UM
20
15
o
o28
†
40
35
25
60
60
pQh
42
dQh
8
o
KaP
14
60
46
10
o
68
56
1
30
25
h
o68
kKmD
35
30
lKtG
30
o
K1G
o
o
45
o
20
36
dQh
o
sJ2-3
Map Description
o
o
o
o
o
o
o
30
o
o
o
o
o o
o
r
s
o
o
25
10
o
o
bJ2-3
o
o
o
o
o
o
o
o
o
vsJ2-3
76
56
26
dQh
h80
50
50
50
80
Kcn-sD
30
36
30
35
sJ2-3
65
o
16
o28 o50
mKcn-mE
30
50
75
70
o40
25
70
52
35
74
dQh
SJ2-3
60
h
o
A
h
o
o
o o
o
o
o
o
o
o
Ks-mG
75
55
15
16
10
o10
h h
o
o
o o
o
†
o
o
o
o
70
tQp
sT1-2
sT1-2
o25
25
Pliocene Fine Sand with Thin Gravelly Intercalations and Lignite Seam
on the Top.
h
o
o
o
o
o
o
o
o
o
sJ2-3
22
15
15
8
o
o
dQh
o15
25
dQp
45
h
o
o o
o
o
o
50
o
o
25
20
KtP
o
h
o
o
o
o
80
fPZ2
50
Np2
60
40
h
18
35
28
o25
lKtG
8
o
o
h
o
o
o
o
o
o
o
40
sJ2-328
15
Gjakovë/Đakovica
Np
o
o
o
o
s
r
o
o
o10
lQp
2
h35
h40
ZO
DANUBIC
M
gNP
40
45
45
Nm
35
35
lQp
Np
15
10
sQp
50
70
lQp
SJ2-3
84
55
Np2
36
45
45
20
64
o75
o75 mKal-cC
o65
46
25
25
h30
60
55
o
70
70
55
35
1
lQp
sJ2-3
o
h
o
o
o
o
o
o
30
o
50
25
ON
GETICU
65
55
70
50
Np1
25
5
Np
60
30
cT1-2
sKmD
lKcn-mC
o50
pQh
25
60
65
Ks-mG
o25 34o
o
2
sJ2-3
30
o80
50
25
pQh
25
35
25
o55
tQp
dQh
50
25
SJ2-3
70
25
60
15
55
!
!
(
NZ
35
o50
65
30
35
SJ2-3
Nm
65
68
63
10
50
30
35
38
o
o
30
o
o
o
o
o
o
35
70
Kv-hC
60
5
25
NE
GO
aEo-Nm
35
56
10
vsT2
h42
Kcn-sD
45
tQp
78
70
58
Np2
40
50
H
Sibiu
!
(
50
Kb-aC
45
40
38
SJ2-3
15
Np1
84
15
40
ZO
S
58
40
80
70
25
kKmD
40
40
8
40
C
AIN
40
52
35
lQp
28
13
40
AN
P A T H O - BAL
o
o
s
r
o
o o
o
o
20
o
65
60
55
42
55
pQh
30
50
o40
70
10 4
h30
25
lQp
N
AN
UNT
H
I
Podujevë/Podujevo
58
Np
Np1
55
Np
70
vpEo-Nm
IA
O
RI M
AT
50
2
80
38
65
35
20
65
52
1
50
sKmD
fKcE
Sarajevo
BR
65
82
75
LI
TE
Adriatic Sea
o
45
40
25
60
20
o
25
30
o
h
o
r
s
s
r
o
o
42
h44
IO
AN
88
o
15
o
rJ2-3
dQh
Np2
45
30
lQp
65
37
Kc-tD
40
45
35
35
o
25
lKtG
o
Np2
kEo
lEo2
35
10
60
60
28
LI
SERBIA
65
10
o10
25
25
40
42
Np
10
o
o
36
sT1-2
o
12
o
o
bJ2-3 nJ2-3
tQp
lT2-3 lT3
30
20
5
tQp
h
o
o
o
o
25
SJ2-3
35
45
10
15
16
o
o
1
sKtG
50
20
20
o
10
o
o
bJ2-3
lQp
o
o
o
25
SJ2-3
SJ2-3
25
12
lQp
65
10
o
o
K1G
sJ2-3
50
30
15
PH
ST
-IV
35
68
20
45
50
12
tQp
Kc-tD
25
o
o
o
15
28
tQp
lKtG 14
o
30
26
o
o
o
20
o
o10
o
o
o
o
o
so
r
r
s
o
Np
Np2
SJ2-3
20
o
o
o
o o
lKmG
2
15
lQp
o
15
20
15
55
o
40
50
27
o
Np
52
o
25
11
1
20
12
Ks-mG
o
60
30
56
56
fyKcn-mE
60
O
48
tQp
38
SJ2-3
50
o
15
40
sKcn-mE
20
30
55
sPZ2
N
!
(
IN
B
! OSN
(
dQh
mKcn-mE
30
54
65
U
75
85
38
78
15
Np
25
35
15
lQp
50
30
25
Nm1
30
45
AP
75
80
75
56
15
1
30
35
o
o
16
25
28
45
40
72
Kb-aC
60
78
tQp
28
55
50
DR
R
EA
25 52
50
o66
o85 Kb-aC
54
50
65
72
45
R-
TE
45
40
45
Vushtrri/Vučitrn
14
25
35
o
40
30
78
52
16
60
30
h
dQh
o62
68
35
85
45
15
20
15
25
45
35
35
25
5
50
30
sKmD
40
o
o
o
sKmG
aQh
gT2
dQh
o
o
o
o
o
o
gQp
o
o
o
o
20
sJ2-3
12
vsJ2-3
lQp
40
o
o
o
sKmG
gQp
50
o
o
o
o
o
h
h
40
20
o
o
o
oo
20
30
rJ2-3
lKtG
50
o25
o
o
lKmG
gQp
40
o
o
15
25
Np1
60
40
25
lT3
50
2
35
40
35
10
45
70
h23
42
bJ2-3
57
52
67
76
82
O
ES
jë
Pe
ra - l
od ersa
k
S h nsv
T ra
55
55
30
50
40
40
40
35
15
20
aQh
o
20
Np2
sT1-2
bPZ
10
60
aQh
75
30
59
10
35
70
30
60
h
45
48
45
SJ2-3
20
45
50
25
70
50
45
10
20
25
30
Ks-mG
ALBANIA
o
o
Np
45
20
o
1
8
30
o
o
Np
20
25
cPZ2
20
o
10
20
25
12
75
15
35
40
58
10
vsT2
60
36
sJ2-3
25
55
58
48
40
65
†
vpEo-Nm
20
20
50
o
50
45
50
48
38
lEo-Nm
20
15
33
50
45
55
40
50
30
22
o
1
lQp
o
h
37
h
nPZ
30
38
25
h
h
h
gQp
Np
30
45
25
bQp
45
1
15
o
h
h
bPZ
Np
pQh
12
h60
1
80
o15
6
40
lQp
vsT2
40
10
o
o
5
7
tQp
lT2-3
50
70
5
10
45
50
35
45
30
20
66
vpJ2-3
35
35
60
40
40
20
h60 sT1-2
Mitrovicë/Mitrovica
45
40
40
40
25
20
Kc-tD o15
52
45
5
10
Np2
27
20
5
10
SJ2-3
15
35
20
25
35
50
25
35
55
20
30
60
50
5
12
38
45
15
10
20
10
10
50
45
Nm
5
o
42
40
20
22
33
39
60
62
30
25
38
vsJ2-3
60
10
o
60
35
o60
72
40
lKcn-mC
52
20
65
35
40
2-3
45
30
lQp
tQp
dQh
ST2
50
mPZ2
h
Np
35
h35
cPZ2
18
Nm
5
45
40
65
64
30
40
dQh
gQp
35
h
35
35
30
o
2-3
15
40
60
40
15
8
aQh
2
dQh
dT1
25
40
bQp
o o
o
lQp
o
gT2
o
gQp
vsT2
bT2
30
40
50
o36
40
50
35
45
20
25
14
50
o
20
30
50
70
5
o
o
h40
bQp
h
30
o
o
55
h20
Np
52
45
56
50
30
o
16
h
40
50
10
10
2
45
45
50
tQp
40
37
30
44
o
h
36
cPZ2
o
h
h37
60
80
40
50
50
50
10
cQp
fPZ2
h65
80
60
30
45
60
60
10
o
Pejë/Peć
IT3
dQh
o
h
45
50
45
40
38
65
42
45
80
o72
16
30
h
75
85
50
lEo-Nm
50
50
20
o45
vsT2
50
o
38
h
50
o
o50
72
h
40
42
lQp
Np
Nm
10
30
o
15
40
10
o26 o
25
o
35
o
o
o
bQp
26
o
o
dT1
lT2-3
o
o
o
38
30
56
70
50
SJ2-3
45
o
bJ2-3
40
42
20
66
o
Nm1
60
22
35
sKmD
50
76
o
h
45
62
58
38
10
35
38
o
kT1
45
vsJ2-3
30
o
o
30
45
2
36
51
35
50
10
aQh
22
65
60
pQh
45
36
o
50
35
o
o
30
50
46
45
30
35
30
SJ2-3
55
o70
55
50
52
48
50
38
W
IT
ZE
50
32
45
12
85
40
Kv-hC
o46
o36
o68
38
45
70
55
50
50
85
32
50
70
Dardanides Cataclastic Bujanovc / Bujanovac Pluton
(with Pegmatitic Veins and Schlieren).
50
60 34
57
SJ2-3
40
Kb-aC
o55
50
55
45
mKcn-mE
o28
55
60
sJ2-3
40
SJ2-3
52
47
60
60
o
o38
40
o
65
60
sJ2-3
40
70
40
45
50
Nm1
60
50
60
SJ2-3
fPZ2
mPZ2
85
30 45
68
vsJ2-3
85
75
45
75
48
35
40
30
vsJ2-3
45
20
45
30
30
47
60
58
80
o
h
h
27
30
o
45
o
35
72
35
50
70
65
30
48
50
45
vsJ2-3
45
cJ2-3
65 o
85
72
o
36
45
o35
42
55
oo
o
55
o
fPZ2
32
o40
o
35
35
35
h
o
lT2-3
30
o
SJ2-3
33
36
o
h
40
30
45
36
54
lT2-3
dT1
25
40
o
lT3
o
o
qPZ2
kT1
60
30
40
lT2-3
kT1
dT1
o50
40
o
o
o
o
o
25
40
30
60
74
60
cJ2-3
25
44
50
45
lEo-Nm
40
o35
30
45
37
60
35
50
50
66
45
80
70
65
40
45
o
48
vsT2
40
45
60
45
60
30
o30
vsT2
35
25
45
o
60
30
40
30
80
Kcn-sD
45
o30
35
50
80
80
50
35
45
40
o
o
o
30
52
47
cPZ2
h30
39
o
o
40
s
r
25
25
40
45
50
o
42
40
50
50
sJ2-3
40
o
o
cPZ2
40
o o
45
sKmD
50
45
45
55
40
55
47
60
vpEo-Nm
nJ2-3
75
SJ2-330
40
sJ2-3
50
vsJ2-3
55
30
20
65
30
57
45
55
45
30
30
o
45
55
o
45
85
bJ2-3
80
60
sKcn-mE
70
52
45
50
o
47
70
30
sPZ2
44
67
47
30
40
30
40
o
58
36
35
45
70
o
39
23
o
45
42
60
89
o
Sharr - Korabi zone (SKZ)
40
bNp
45
lEo-Nm
75
45
45
55
75
37
o
o
o
TKO
42
30
lEo-Nm
67
50
†
50
60
50
60
60
28
o
70
65
†
60
25
o
MKC
MKC
22
sJ2-3
70
o
vpEo-Nm
MONTENEGRO
48
35
60
65
o35
gPZ2
50
70
vsT2
o o70
65
MNB
25
Ophiolite belt (OB)
45
o
Miocene Tuffs with Bombs.
JBR
CPA
o
65
CBKA
CBDS
CKC
APZ2
55
CBKM
MSH
40
o55
bJ2-3
45
25
o
CJE
JGJ
65
lEo-Nm
o
50
CBKK
CVNK
h60
50
20
MNB
JKZ
CVNK
MGA
MST
CBDG
CVT
40
o
CBMI
JRA
CBKO
50
aEo-Nm
RM
20
70
80
h h
JGO
o
DA
CPG
CCA
60
CVBK
CVBK
DU
45
55
aEo-Nm
h
MKU
o65
gPZ2
CBKS
CCA
CBDU
50
Beograd
lEo-Nm
55
o55
20
sKcn-mE
vsJ2-3
35
Nm
80
vs
Leposaviq/Leposavić
50
Kcn-mD
SJ2-3
55
o
CVT
CBDR
50
APZ2
h
CBDP
40
mPZ2 vpEo-Nm
Dardania massif (DM)
(Serbo-Macedonian massif)
TKR
sJ2-3
aEo-Nm
nJ2-3
h
TMO MRU
vsJ2-3
CVMB
CVMS
o
45
Internal Vardar subzone (IVZ)
CBPO
Pleistocene River Terrace of the River Sitnicë / Sitnica.
20
sJ2-3
h
JST
45
30
h
60
JLE
TKU
CZU
o
60
MJK
MKO
45
o
SJ2-3
CVKB
o20
35
vsNm
26
35
E
ALIF
CA
R
o
vsJ2-3 80
60
East Bosnian - Durmitor zone (EBDZ)
35
70
35
o
o
o
MET
lEo-Nm
o
4780000
aQh
45
o
o30
Szeged
!
(
RP
AT
h
o
o
80
vpEo-Nm
TRANSYLVANIAN
BASIN
NI S
S E AI N
U
A P UNT
O
M
RP
I
nJ2-3
sJ2-3
75
CA
NE
o
80
35
R
sJ2-3
PANNONIAN BASIN
aEo-Nm
25
50
CA
PE - FLYSCH Z
NAP
O
vpEo-Nm
75
30
o
bJ2-3
JLE
20
NE
S
aEo-Nm
Central Vardar subzone (CVZ)
CVRB
20
40
vsNm
lEo-Nm
External Vardar subzone (EVZ)
Drin-Ivanicki element (DIE)
aEo-Nm
50
35
IN
h
sJ2-3
AN
Koritnik Triassic unit
Moknes-Alpet Shqipetare Triassic complex
Çiçavica Triassic unit
Kutlovc Triassic unit
Kolashin metamorphic unit
Sharr metamorphic complex
Shtime metamorphic unit
Gadima metamorphic unit
Kaçanik metamorphic unit
Rugovë metamorphic unit
Novobërdë metamorphic unit
Kurolai metamorphic unit
Kopaonik metamorphic footwall unit
Dardania massif (Serbo-Macedonian massif)
S
-
HI
TKO
TMO
TKR
TKU
MKO
MSH
MST
MGA
MKC
MRU
MNB
MKU
MJK
DA
Drenicë Cenozoic basin
Mirushë Cenozoic basin
Pashtrik Upper Cretaceous syncline
Pagarushë Upper Cretaceous anticline
Carralevë Upper Cretaceous unit
Jezerka Upper Cretaceous unit
Kaçanik Upper Cretaceous unit
Zubin Potok Upper Cretaceous unit
Vardar Lower Cretaceous flysch trough
Brezovicë Jurassic ophiolitic complex
Gjakovë Jurassic peridotite complex
Golesh Jurassic ophiolitic complex
Koznicë Jurassic ophiolitic complex
Strofc Jurassic ophiolitic unit
Leposaviq Jurassic ophiolitic complex
Rahovec Jurassic ophiolitic complex
Scale approx. 1 : 5,000,000
IT E
AN
RG
- HA
A N T A IN S
L IM
CA M OUN
-
o
CBDR
CBMI
CPA
CPG
CCA
CJE
CKC
CZU
CVT
JBR
JGJ
JGO
JKZ
JST
JLE
JRA
CVKB
(
7560000
Geotectonic Units of Central Balkan Peninsula
mPZ2
JLE
(
( (
7550000
4760000
55
o
Badofc/Kishinca Cenozoic volcanic complex
Kopaonik/Belobërdë Cenozoic volcanic complex
Majdan/Braine Cenozoic volcanic complex
Mitrovicë/Samadrexhë Cenozoic volcanic complex
Nosale-Kllokot Cenozoic volcanic complex
Rogoznë/Bube Cenozoic volvanic complex
Dukagjin Cenozoic basin
Gjakovë Cenozoic subbasin
Pejë Cenozoic subbasin
Suharekë Cenozoic subbasin
Kamenicë Cenozoic basin
Moravë Cenozoic subbasin
Kriva Rekës Cenozoic subbasin
Strezofc Cenozoic subbasin
Kosovo Cenozoic basin
Podujevë Cenozoic basin
(
7540000
gdNm
Scale approx. 1 : 1,200,000
o
-
7530000
21°0'0"E
Regional Geological Units of Kosovo
CVBK
CVKB
CVMB
CVMS
CVNK
CVRB
CBDU
CBDG
CBDP
CBDS
CBKA
CBKM
CBKK
CBKS
CBKO
CBPO
7520000
h
20°0'0"E
7510000