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Geology Of Kurdistan, Iraq
Saad Z Jassim Heritage Oil
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Northerly Movement of the Arabian Plate
20Ma-Present Volcanics Arabian Plate Northerly movement of the Arabian Plate resulted in collision with the Anatolian Plates first producing the E-W trending anticlines followed by the stress introduced against the Iranian Plates in NE-SW direction resulting in NW trending anticlines of NE Iraq; some are overprinted over the Anatolian trend in N Iraq
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Arabian Plate Boundary
Dismembered Oceanic Crust Iranian Plates Arabian Plate
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Regional geology
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Boundary of The High Folded Zone in Qara Dagh and Bazian
25 My 8 My 50 My 55-60 My Chemchemal Qara Dagh
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Miran profile along seismic line 5
Line HEML-08-05
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Bazian Anticline
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Sara Anticline
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Injana (U Fars) Formation (U Miocene) near Erbil
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Bazian North L Fars Pila Spi U Fars
Gypsum Quarries L Fars Pila Spi U Fars Bazian North Fatha (L Fars Formation) Formation (M Miocene) along SW limb of Bazian North
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Fatha (L Fars ) Formation (M Miocene) :Thickness ~300m near Miran
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Pila Spi Formation (U Eocene) on SW limb of Bazian
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Gercus Formation (M Eocene) in southern part of Miran reaches 130m
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Sinjar Formation (L Eocene) totals 220m in Miran
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Kolosh Formation (M-U Palaeocene) ~700m in Miran
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Tanjero Formation (Campanian-Maastrichtian) ~100m in Miran W, 800 in Miran E, 1500m in Pira Magrun and over 2000m to the east and southeast of Sulaimaniya
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Shiranish Formation (Campanian-Maastrichtian) near Dokan (two distinct parts). Reaches >430m in Miran-1
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Kometan Formation(Turonian) in SW limb of Pira Magrun
Kometan Formation(Turonian) in SW limb of Pira Magrun. Reaches 160m in Miran-1
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Dokan Formation (Cenomanian) near Dokan (two distinct parts)
Dokan Formation (Cenomanian) near Dokan (two distinct parts). 8m thick near Dokan but not recognised in Miran wells
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Balambo Formation At Jabal Azmur East Of Sulaimaniya (~800m)
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Other possible ramp to the east?
Facies Change From Qamchuqa (NW) To Balambo (SE) Along Pira Magrun Other possible ramp to the east? N Qamchuqa Ramp facies Balambo Outer gentle slope Steep Slope facies
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Kometan/Qamchuqa/Sarmord Formations In Middle Section Of Pira Magrun
Slope facies
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Balambo Formation (Berriasian-L Turonian) up to 800m near Sulaimaniya, 440m in Miran
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Balambo Formation (Berriasian-Early Turonian) slope facies in Jabal Azmur
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Qamchuqa Formation (Aptian-Albian) in Geli Tabin on NW plunge of Pira Magrun (Top) vuggy coarse-grained dolomite and Jabal Sara (right)
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Passage of Qamchuqa steep slope facies (massive beds) into Balambo (thin-bedded) in the Central and SE part of Pira Magrun as seen from Zewi springs
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Sarmord Formation (Valanginian-Barremian) in Zewi gorge ( ~360m in Miran)
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Geological Map Of The Surrounding Of Ranya Town
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Barsarin and Chia Gara)
The Jurassic Section Near Ranya Town M-U Jurassic (Sargelu-Naokelekan Barsarin and Chia Gara) Aptian-Albian Qamchuqa L Jurassic (Sarki & Sehkaniyan) L Cretaceous Sarmord Ranya Town
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Qamchuqa Sarmord Chia Gara (Tithonian-Berriasian) View NW From Barsarin Village, NE of Erbil ( <100m in Miran)
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Barsarin (U Jurassic) Naokelekan (M Jurassic) Barsarin (U Jurassic) and Naokelekan (M Jurassic), Barsarin Village, NE of Erbil
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Sargelu (M Jurassic), Barsarin Village, NE of Erbil
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Inliers (imbricates) of the Liassic Sehkaniyan Formation (Alan-Mus-Adaiyah and part of Butmah-equivalent) within the obducted Aptian-Albian Qulqula Radiolarian Chert
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Northern Iraq
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Northern Part Of NE Iraq
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Southern Part Of NE Iraq
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