LITHOSTRATIGRAPHIC STUDY OF A LATE OLIGOCENE – EARLY MIOCENE SUCCESSION, SOUTH OF SULAIMANIYAH, NE IRAQ Polla A. Khanqa, Kamal Haji Karim, Sahira A. Karim, Varoujan K. Sissakian Publish in : Iraqi Bulletin of Geology and Mining Vol.5, No.2, 2009, p 41− 57 ABSTRACT Late Oligocene–Early Miocene rocks are not previously known in […]
ORIGIN OF LIMESTONE CONGLOMERATE IN DOKAN (Dukan) AREA, KURDISTAN REGION, NORTHEAST IRAQ By: Kamal Haji Karim and Zardasht Ahmad Taha, University of Sulaimani published in: Iraqi Bulletin of Geology and mining, Vol.2, No.3, p.15-24, 2012 Abstract Thick succession of limestone conglomerate (about 300m thick) is exposed on right and left sides of Dokan […]
History and Geological Setting of Intermontane basin in the Zagros Fold-thrust belt, Kurdistan Region, NE-Iraq Department of Geology, University of Sulaimani KAMAL H. KARIM , SHERZAD Tofiq Al-BARZINJY AND BAKHTIAR, M. Ameen Received: 20/3/2007, Accepted: 13/ 9/ 2007 Published in: Iraqi Bulletin of Geology and mining, Vo.4,No.1, 2008 ,p21-33 Abstract It is mentioned […]
Historical development of the present day Lineaments of The western Zagros Fold-Thrust belt: a case study from Northeastern Iraq, Kurdistan Region Kamal H. Karim Amanj Ibrahim Fatagh Azad Ibrahim Department of Geology Department of Geology Department of Geology College of science College of science College of science University of Sulaimani […]
TECTONICAL HISTORY OF ARABIAN PLATFORM DURING late CRETACEOUS: AN EXAMPLE FROM KURDISTAN REGION, NE-IRAQ Kamal H. Karim* and Zardasht A. Taha* *University of Sulaimani, Department of Geology Published in: Iranian Journal of Earth Sciences 1 (2009) / 1-14 Abstract New simplified tectonic models and depositional history of Late Cretaceous rocks are established […]
NEW IDEAS ABOUT GULNERI SHALE FORMATION (EARLY TURONIAN) IN DOKAN AREA, KURDISTAN REGION, NE IRAQ Zardasht A. Taha and Kamal H. Karim, University of sulaimani Published In: Iraqi Bulletin of Geology and Mining, Vol.5, No.2, 2009,p29-39 ABSTRACT Gulneri Formation (Early Turonian) consists, mainly as previously described, of shale deposited in euxinic and small relic […]