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Prishtinë/PrištinaPejë/Peć
Ferizaj/Uroševac
Prizren/Prizren
Gjakovë/Đakovica
Mitrovicë/Mitrovica
Gjilan/Gnjilane
Vushtrri/Vučitrn
Podujevë/Podujevo
Leposaviq/Leposavić
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20
2025
2017
15
15
20
25
25
35
35
20
18
35
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2825
6050
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2525
70
70
65
7080
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20
45
60
4570
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35
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15
30
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15
10
23
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2015
70
70
70
65
80
80
7080
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50
70
70
85
80 80
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60
70
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82
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55
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42
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50
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55
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35
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2015
17
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2020
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34
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35
60
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50
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30
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50
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55
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50
70
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40
30
60
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50
60
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7420000
7420000
7430000
7430000
7440000
7440000
7450000
7450000
7460000
7460000
7470000
7470000
7480000
7480000
7490000
7490000
7500000
7500000
7510000
7510000
7520000
7520000
7530000
7530000
7540000
7540000
7550000
7550000
7560000
7560000
4
5900
00
4
5900
00
4
6000
00
4
6000
00
4
6100
00
4
6100
00
4
6200
00
4
6200
00
4
6300
00
4
6300
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4
6400
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4
6400
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4
6500
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4
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4
6600
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4
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4
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4
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4
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4
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4
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4
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4
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4
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4
7400
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4
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4
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4
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4
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7700
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4
7700
00
4
7800
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4
7800
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4
7900
00
4
7900
00
20°0'0"E
20°0'0"E
21°0'0"E
21°0'0"E
42°0
'0"N
42°0
'0"N
43°0
'0"N
43°0
'0"N
Scale 1 : 200,000GEOLOGICAL MAP OF KOSOVO
MACEDONIA
bQp
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νJ2-3 νJ2-3
νJ2-3
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σJ2-3
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smKcn-mC
smKcn-mC
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lKcn-mC
lKcn-mC
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mKal-cC
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Kv-hC
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smJ2-3
cJ2-3
smJ2-3
smJ2-3
sJ2-3
sJ2-3
cJ2-3
cJ2-3
AJ2-3
AJ2-3
cT1-2
sT1-2
sT1-2
sT1-2
sPZ2
fPZ2
fPZ2
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ALBANIA
MONTENEGRO
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dQh
dQh
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0510152025
Rahovec Ophiolite Complex (Basalt Pillows and Plagio-Rhyolite).Folded Upper Cretaceous Platy Limestone (Carbonate Platform).
Miocene Tuffs with Bombs.
Pleistocene River Terrace of the River Sitnicë / Sitnica.
High-Grade Metamorphic Rocks (Migmatitic Gneiss) in the KaçanikMetamorphic Unit.
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Pliocene Fine Sand with Thin Gravelly Intercalations and Lignite Seamon the Top.
Scale approx. 1 : 1,200,000Regional Geological Units of Kosovo
Sharr - Korabi zone (SKZ)
Ophiolite belt (OB)
East Bosnian - Durmitor zone (EBDZ)
Drin-Ivanicki element (DIE)
External Vardar subzone (EVZ)
Central Vardar subzone (CVZ)
Internal Vardar subzone (IVZ)
Dardania massif (DM)(Serbo-Macedonian massif)
DA
CJE
MNB
JLE
CCA
CVT
JLE
JLETKU
MJK
MGA
CVT
JKZ
MNB
MKC
MKC
CKC
JBR
TKO
CPA
MSH
MST
JGO
JRA
TKR
CPG
CCA
CZUMKO
JST
MRUTMO
MKU
CBKM
CBKS
CBKK
CVKB
CVKB
CVMSCVMB
CVBK CVBK
CVNK
CVNK
CVRB
CBDP
CBDS
CBDG
CBMI
CBDR
CBKO
CBPO
CBDU
CBKA
JGJ
CBDR - Drenicë Cenozoic basinCBMI - Mirushë Cenozoic basinCPA - Pashtrik Upper Cretaceous synclineCPG - Pagarushë Upper Cretaceous anticlineCCA - Carralevë Upper Cretaceous unitCJE - Jezerka Upper Cretaceous unitCKC - Kaçanik Upper Cretaceous unitCZU - Zubin Potok Upper Cretaceous unitCVT - Vardar Lower Cretaceous flysch troughJBR - Brezovicë Jurassic ophiolitic complexJGJ - Gjakovë Jurassic peridotite complexJGO - Golesh Jurassic ophiolitic complexJKZ - Koznicë Jurassic ophiolitic complexJST - Strofc Jurassic ophiolitic unitJLE - Leposaviq Jurassic ophiolitic complexJRA - Rahovec Jurassic ophiolitic complex
TKO - Koritnik Triassic unitTMO - Moknes-Alpet Shqipetare Triassic complexTKR - Çiçavica Triassic unitTKU - Kutlovc Triassic unitMKO - Kolashin metamorphic unitMSH - Sharr metamorphic complexMST - Shtime metamorphic unitMGA - Gadima metamorphic unitMKC - Kaçanik metamorphic unitMRU - Rugovë metamorphic unitMNB - Novobërdë metamorphic unitMKU - Kurolai metamorphic unitMJK - Kopaonik metamorphic footwall unitDA - Dardania massif (Serbo-Macedonian massif)
- Kopaonik/Belobërdë Cenozoic volcanic complexCVKB- Majdan/Braine Cenozoic volcanic complexCVMB- Mitrovicë/Samadrexhë Cenozoic volcanic complex CVMS- Nosale-Kllokot Cenozoic volcanic complexCVNK- Rogoznë/Bube Cenozoic volvanic complexCVRB- Dukagjin Cenozoic basinCBDU- Gjakovë Cenozoic subbasinCBDG- Pejë Cenozoic subbasinCBDP- Suharekë Cenozoic subbasinCBDS- Kamenicë Cenozoic basinCBKA- Moravë Cenozoic subbasinCBKM- Kriva Rekës Cenozoic subbasinCBKK- Strezofc Cenozoic subbasinCBKS- Kosovo Cenozoic basinCBKO- Podujevë Cenozoic basinCBPO
- Badofc/Kishinca Cenozoic volcanic complexCVBK
Geotectonic Units of Central Balkan Peninsula Scale approx. 1 : 5,000,000
1 : 200,000
0 5 10 15 20 25Kilometres
Triassic Metasandstone (Left Side) and Metadiabase (Right Side,in the Foreground).
!
!
!!
!
!
!
!
!
!
!!
!
!
!
!
! !
! !
!
!
!!
!
!
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!
!
!(
!(
!(
!(
!(
!(
!(
!(
!(
DURMITOR-EAST BOSNIAN ZONE
DINARIDES HELLENIDES
APULIAN ZONE
DALMA
TIAN
-HER
ZEGOVINIA
N ZONE
IONIAN ZO
NE
PANNONIAN BASIN
WESTERN OPHIOLITE BRANCH
PELAGO
NIAN MASSIF
VARDAR ZONE
EASTERN OPHIO
LITE BRANCH
SERBO-M
ACEDONIAN M
ASSIF
RHODOPE MASSIF
SREDNA GORA
MOESIAN PLATFORM
GE
TICU
M
DANUBICUM
Adriatic SeaAegean Sea
Shkodra-Pejë
Transversal
CARPATHIANS
BALKANIDES
KRAIŠTID
ES
STARA PLANINA ZONEFORE BALKAN
CARPATHIANS FOREDEEP
TRANSYLVANIANBASIN
GETICUM
METALIFERI MOUNTAINS
KORABI ZONE
KRASH
TA - ÇUKALI ZONE
Beograd
Sofia
Prishtinë
Skopje
Sarajevo
Tirana
Szeged
Sibiu
Bucureşti
MIR
DITA O
PHIO
LITE BRANC
H
INNER CARPATHIANS
CALIM
AN - H
ARG
ITEI
MO
UN
TAINS
DRIN-IVANICKI ELEMENT
CARP
AT
HO
- BA
LKAN ARC
NAPP
E - F LY
SC
H ZONE
KRUJA - GAVR
OVO
ZON
E( SUBPELAGO
NIAN ZONE )
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 V
V V V
V V V
V V
V V V
V
V V
V
KK K
K K
K KK K
K Kv v v v
V
v v v
v v v v
D
D
D D D D D D D
D D D D D D
Á Á Á Á Á
Á Á Á Á Á Á
Á Á Á Á
Á Á Á Á ÁÁ Á Á Á Á ÁÁ Á Á Á Á Á Á ÁÁ Áv v
v
v
v vv v v
v
v v
V
V V V V V V V
K K KK
K K KK K K
V V
K K K KK K K
V V V
v vv vK K K
K K K
V V
V VK K KK K K
K KK K v v
v v
K K K
B
Mirushë Cenozoic basin
Denac
Drenicë Cenozoic basin
Lumi i Badlavës
A
Drini i Bardhë
DRIN - IVANICKI ELEMENTExternal Vardar subzone
VARDAR ZONECentral Vardar subzone Internal Vardar subzone
DARDANIA MASSIF
Gjakovë Jurassicperidotite complex
OPHIOLITE BELT
Proni i Beces
Rahovec JurassicOphiolite complex
Pagarushë UpperCretaceous anticline
CarralevëUpper Cretaceous unit
Çiçavica Triassic unit
Lumi i Sitnicës
Kosovo Cenozoic basin Vardar Lower Cretaceous Flysch trough Majdan / Braine Cenozoicvolcanic complex
σJ2-3 Np2
KaP σJ2-3
SW
1000
0
- 1000
m aslErenik tQp Mirushë
NE
1000
0
- 1000
m asl
Schematic Geological Cross Section across Kosovo Scale 1 : 200,000
Dukagjin basinGjakovë Cenozoic subbasin
Np2
aQh aQhβJ2-3
σJ2-3dQh
K1GNp1 tQp
vsJ2-3 sKtG
lKtGKs-mG
Np1lQp
lKtG Ks-mG
sKmD smJ2-3Kcn-sD
SJ2-3
Np1
tQp sKmD Np1
σJ2-3 smKcn-mC
aQh tQppQh
sJ2-3
dQh
smKcn-mC
mKcn-mE mKal-cC Kb-aC
Kv-hC
vpEo-Nm αEo-Nm gNPcT1-2sT1-2
ρJ2-3
σJ2-3ρJ2-3
SJ2-3
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.
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.
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.
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.
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.
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.
Selected Literature and Sources of Data GEOLOŠKA KARTA SR SRBIJE, 1 : 200,000 Beograd 1968, Zavod za Geološka i Geofizička Istraživanja, Languages: Serbo-Croatian and French).
GEOLOGICAL MAP OF YUGOSLAVIA, 1 : 500,000 (printed 1971, 6 map sheets).
GEOLOŠKO-TEKTONSKA KARTA SAP KOSOVO, 1 : 100,000, Zagreb 1974, Geozavod Zagreb, Language: Serbo-Croatian.
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: Serbo-Croatian).
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
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.
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.
The oldest core of the Balkan Peninsula is situated within the Circum Rhodope belt with medium- to high-grade-metamorphic 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.
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.
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 volcanic-sedimentary 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).
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.
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.
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 / Serbo-Macedonian 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.
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.
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.
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).
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.
Map Description
r
rÁ Overturned axis, syncline
Ás
s Overturned axis, anticline
Fault, observed
� Axis of fold
Dip of axis syncline and of anticline
Fault, indicated
Front of overthrust, observed
Front of overthrust, indicatedo30 Bedding, normal, dip of bedding
Foliation, normal, dip of foliationh
45
Constructional area(cities, villages, etc.)
Main road
Regional road
Railway
River
Water reservoir
Line of cross sectionA B
sr
Axis of syncline
rs
Axis of anticline
Geological boundary, observed
Boundary with lithological transition zone (indefinite boundary)
Geological boundary, indicated
Boundary of olistolith
Lower Miocene
Nm18 88 8
8 8(
(
( Conglomerate, sandstone, claystone
Upper Oligocene
PALAEOGENEOligocene
Lower Oligocene
lEo1 Reef (corals) limestone8 8
8 8 8
8 8 8
claystone, partly limestone, pyroclastic rocksConglomerate, sandstone, marlstone, kEo1
oo
oo
N NN
N(
( (
Coniacian - Maastrichtian
CRETACEOUSPASHTRIK CRETACEOUS (P)
PAGARUSHA CRETACEOUS (G)Maastrichtian
Sandstone, conglomerate (flysch)N N
N N
N N N( (
( (
( (
sKmG
lKmG
8 8
8 8
8 8 8 Rudist limestone
Santonian - Maastrichtian
Ks-mG Thin-bedded limestone with cherto oo oo o
Turonian
lKtG
8 8
8 8
8 8 8 Massive sandy limestone with Rudists
sKtG< < << < << < < Clastic sediments with diabase fragments -
sedimentary mélange
Turonian
KtP8 8
8 8 8 Sandy limestone with Rudists
Cenomanian
KcP( (
( (
o o oo o oo o Conglomeratic banked limestone
Aptian - Cenomanian
Ka-cP Thin-bedded limestone, calcarenite8 8
8 8 8
8 8 8
Aptian
KaP Conglomerate, chert, sandstoneN N
N N
N N N( (
( (
8 88 8
8 8o oo oo o
Kcn-mP Limestone, marlstone, calcarenite with chert
lEo2
88
88 8
8 8
8
8 888 Limestone, partly marly and dolomitic
sEo28 8
8 88 8 Sandstone, marlstone, mudstone, partly
tuffitic, magnesite and lignite bearing
kEo2. .
. . .Conglomerate
Middle - Upper Miocene
Nm2-3(
( (
8 88 88
8o
o oo o
Gravel, sand, clay, marl, marly limestone
Upper Miocene
Nm3N N N
N N NN N Sandstone, marlstone, mudstone
Miocene
Nmoo
o oN N
N NN
( (
(
Conglomerate, sandstone,marlstone, claystone
Middle Miocene
mNm2
8 8 8
8 8 8
8 8 8
Marlstone, claystone, sandstone, partly tuffstone and lignite
kNm2N N N
N N N
N N( (
( (
( (
Gravel, sand, sandy clay, tuffs
sNm2NN Noo o Sandstone, conglomerate,
claystone, limestone, tuffs
Lower Pliocene
Np1(
(
(8 8 8o oo oo o
Clastic sediments, clay, sand, gravel,marl, carbonate lenses, burnt rock, lignite
Upper Pliocene
NEOGENEPliocene
Np2
8 88 8
88(
( (
( ( Clastic sediments, clay, sand, gravel,partly marl, tuffite
Pleistocene
gQp³³ ³ ³³ ³³ ³³ ³³
³³ ³³ ³³ ³ ³³ ³
³³ ³³ ³³ ³ ³³ ³ Glacigene sediments - moraine, fluvio- and limnoglacial deposits
lQp Lake sediments - gravel, sand, silt, clay8 8 88 8 88 88 8 tQp River terraces - gravel, sand(
( (
(
(
( (
( (
( (
( (
(
cQp Calc tufa / travertine
ø ø
ø ø
ø ø
ø ø
Legend
HoloceneQUATERNARY
pQhr
r
(
( ( Proluvium - fanglomerate of rock fragments,sandy-silty deposits
dQh Deluvium - rock fragments, sand, siltr r
r
r
aQh Alluvium - gravel, sand, silt( (
( (£ ££ £ ££ £ £
Coniacian - MaastrichtianCENTRAL VARDAR ZONE (C)
Cenomanian
fKcEK K K KK K K K
K K KK K KK K K
Phyllite, calcareous schist
Lower Cretaceous
K1G8 8 8
8 8 Reef limestone, limestone breccia
Aptian - Cenomanian
kKal-cC( ( (
( (
( (Conglomerate, sandstone (flysch)
mKal-cCo oo oo o Marlstone, limestone, sandstone,
siltstone (flysch)
smKcn-mC Sedimentary mélange< < << < << < << < <
Massive coralliferous limestone8 8 8
8 8 8
8 8 bKcn-mC
lKcn-mC8 88 8
8 8o o
o oo o Limestone, marlstone, chert, calcarenite,
partly conglomerate (calcareous flysch)
DRIN - IVANICKI ELEMENT (D)Maastrichtian
kKmDN N N
N N( ( (
( (
Sandstone, conglomerate (flysch)
sKmDN N N
N N N
N N( ( (
( (
( (
Sandstone, siltstone, marlstone (flysch)
Coniacian - Santonian
Kcn-sD8 8 8
8 8
8 8
Reef and Rudist limestone
Coniacian - Maastrichtian
Kcn-mDo oo oo o Limestone, marlstone, siltstone
(calcareous flysch)
EXTERNAL VARDAR ZONE (E)Coniacian - Maastrichtian
fyKcn-mEo oo o
(calcareous flysch)Limestone, marlstone, siltstone
mKcn-mE8 8 8
8 8
8 8 Marlstone, limestone
sKcn-mEN N NN N
N N
conglomerate, marlstone, limestoneSandstone, siltstone,
Kcn-mE. . .. . Conglomerate
Cenomanian - Turonian
Kc-tD Conglomerate, breccia, sandstone, limestoneoo oo o
(
(
( (
bQp Boulder field
(ØØØØØ
(ØØØØØ
(ØØØØ
(ØØØØ
(ØØØØØ
(ØØØØØ
(ØØØØØ
(ØØØØØ
NEOPROTEROZOIC
gNPK K K
K K KK K K
K K KK K K
K K K
K K K
K K K Mainly gneiss, subordinately mica schist, leptite and granulitic rocks
mNPK K K K
K K K K
K K K K
K K K
K K KMainly mica schist, subordinately gneiss
MNPK KK K
K K| |
| |
| |Mainly migmatitic rocks, partly granulitic,subordinately different gneiss
qNP Quarzite!( !( !(
!( !( !(
!( !( !( !(
!( !( !( !(
ANP Amphibolite
Lower Palaeozoic
fPZ1K K KK K K
K K K KK K K KK K K K
Phyllites
Quarzite, meta-conglomerateqPZ1!( !( !(
!( !( !( !(
!( !( !( !(
sPZ1KKKKKKKKKKKKKKKKKKKK
Epidote - chlorite - and actinolite schist,partly diabase, with marble intercalations
mPZ1K K K K
K K K KK K K
K K KBiotite muscovite schist
gPZ1K K K
K K KK K K
K K KK K K
K K K
K K K
K K K Biotite gneiss, leptinitic gneiss
APZ1 Amphibolite
cPZ1 Marble
PALAEOZOICUpper Palaeozoic
qPZ2 Quartzite, meta-sandstone, meta-conglomerate!( !( !(
!( !( !(
!( !( !( !(
sPZ2K K KK K K
K K KK K K
Greenschist, phyllite, mudstone, chert
fPZ2K K KK K KK K K
K K K KK K K K Phyllites, sericite schist, quartz schist,
meta-sandstone
mPZ2KKKKKKKKKKKKKKKKKKKK
Epidote schist, actinolite chlorite schist,partly muscovite schist, diabase
gPZ2K K K
K K K
K K K
K K KK K K
K K KK K K Biotite gneiss, biotite schist,
with marble intercalations
cPZ2 Marble, recrystallised cherty limestone
APZ2 Amphibolite, amphibole schist
CENOZOIC MAGMATIC EVENTOligocene - Pliocene
vpEo-NmÁ Á Á Á
Á Á Á Á
Á Á Á ÁÁ Á Á Á Pyroclastic rocks
RhyoliteD D
D D
D D D πEo-Nm
τEo-NmD D D D
D D D D
Trachyte
βNp Basalt
V V V V
γδNm GranodioriteÎ Î Î Î
Î Î Î ÎÎ Î Î
λEo-Nm LatiteD D D D D
D D D D D
D D D D D
αEo-Nm AndesiteD D D D
D D D D
vsNm Volcanic-sedimentary seriesv v vv v
Middle - Upper JurassicJURASSIC MAGMATIC EVENT
vsJ2-3 Volcanic-sedimentary seriesv v vv v
v v
βJ2-3 BasaltV V V
V V V
vpJ2-3 Pyroclastic rocksÁ Á Á Á
Á Á Á Á
Á Á Á ÁÁ Á Á ÁÁ Á Á Á
γJ2-3 Granitic rocksÎ Î Î
Î Î Î
Î Î! ! !
! !
GranodioriteγδJ2-3Î Î Î
Î Î Î! ! !
νJ2-3 Gabbro
V V V V
V V V V
σJ2-3 Peridotite, dunite, partly serpentinised
V V
ρJ2-3 Pyroxenite, partly serpentinisedV V
SJ2-3 SerpentiniteV V
V V
Middle TriassicTRIASSIC MAGMATIC EVENT
vsT2 Volcanic-sedimentary seriesv v
v v v
βT2 Meta-basalt
V V V
V V V
γT2 Granite, meta-graniteÎ Î
Î Î Î
Î Î Î
ST2 Serpentinite
V
V V
PALAEOZOIC MAGMATIC EVENT
πPZ Meta-porphyry, meta-keratophyreD D D
D D D
βPZ Meta-basalt
V V V
V V V
γPZ Meta-granitic rocksÎ Î Î
γδPZ Meta-granodiorite, meta-dioriteÎ Î Î
Î Î Î
Meta-syeniteζPZÎ Î Î
Î Î Î
νPZ Meta-gabbroV V V
V V V
Valanginian - Hauterivian
Kv-hCoo oo o
(
( ( Conglomerate, sandstone,siltstone, partly limestone
Barremian - Aptian
Kb-aCN N
N N N( (
( ( Sandstone, siltstone, conglomerate, partly marlstone (flysch)
Middle - Upper JurassicJURASSIC
sJ2-3K K KK K K
K K KK K K
schists, phyllites, gneissesMeta-sedimentary silicate rocks -
smJ2-3< < < << < << < <
Tectonic mélange with olistoliths - limestone, schists, volcanic rocks
cJ2-3 Meta-carbonate rocks - marbles, calcschists
AJ2-3 Orthometamorphic rocks -amphibolite - metamorphic sole
Lower Triassic
dT1888 888 Limestone, dolomite
kT1N N
N N
N N N( (
( (
( (
Conglomerate, sandstone, mudstone, breccia
Upper Triassic
lT3 Cherty limestoneo o oo oo o
TRIASSIC
lTo o oo o oo o Olistoliths of cherty limestone
(uncertain age)
Lower - Middle Triassic
sT1-2K K KK K KK K KK K K
Meta-sedimentary silicate rocks -schists, quartzite, meta-conglomerate
cT1-2 Meta-carbonate rocks -marbles, calcareous schists
Middle - Upper Triassic
Limestone, dolomite, partly chertylT2-3
8 8
8 8
8 8 8
APUSENI
MOUNTAINS
Dardanides Cataclastic Bujanovc / Bujanovac Pluton(with Pegmatitic Veins and Schlieren).
vsT2
November 2006
Beak Consultants GmbHAm St. Niclas Schacht 1309599 Freiberg, GermanyManaging director: A. Barthwww.beak.de
Independent Commission for Mines and MineralsKomisioni i Pavarur për Miniera dhe MineraleNezavisna Komisija za Rudnike i Minerale
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 isintended 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 oninternational boundaries.
Magnetic Declination3.3° E
Vector data basedon Topographical mapsof former Yugoslavia 1 : 50,000edition 4-NIMA, series M709.Copyright 1998 by the United States Government. No copyright claimed under title 17 U.S.C.
Topography
E. Dickmayer, A. KnoblochCartography / GIS
A. Knobloch, C. LeglerScientific processing
Transverse mercatorMap projection
Based on Osnovna Geološko KartaSFRJ 1 : 100,000 - Geološki Institut, Beograd (1970-1984).
Geology / Lithology
Ellipsoid: Bessel 1841Datum: MGI Austria
Reference system
Governing BoardRr. Rrustem Statovci 29Prishtinë, KosovoChairman: Naip Zekawww.kosovo-mining.org
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