M. Ghafor, I. (2011). MICROFACIES AND BIOSTRATIGRAPHY OF BABA FORMATION (LATE OLIGOCENE) IN BAI HASSAN, OIL WELL-25, KIRKUK AREA, CENTRAL NORTH IRAQ. , 7(3), 25-32.
Imad M. Ghafor. "MICROFACIES AND BIOSTRATIGRAPHY OF BABA FORMATION (LATE OLIGOCENE) IN BAI HASSAN, OIL WELL-25, KIRKUK AREA, CENTRAL NORTH IRAQ". , 7, 3, 2011, 25-32.
M. Ghafor, I. (2011). 'MICROFACIES AND BIOSTRATIGRAPHY OF BABA FORMATION (LATE OLIGOCENE) IN BAI HASSAN, OIL WELL-25, KIRKUK AREA, CENTRAL NORTH IRAQ', , 7(3), pp. 25-32.
M. Ghafor, I. MICROFACIES AND BIOSTRATIGRAPHY OF BABA FORMATION (LATE OLIGOCENE) IN BAI HASSAN, OIL WELL-25, KIRKUK AREA, CENTRAL NORTH IRAQ. , 2011; 7(3): 25-32.

MICROFACIES AND BIOSTRATIGRAPHY OF BABA FORMATION (LATE OLIGOCENE) IN BAI HASSAN, OIL WELL-25, KIRKUK AREA, CENTRAL NORTH IRAQ

Iraqi Bulletin of Geology and Mining
Article 1, Volume 7, Issue 3, 2011, Pages 25-32
Author
Imad M. Ghafor
Abstract
Larger Foraminifera in the Baba Formation (Middle Oligocene) are discussed. The investigation is based on a well sequence of limestone in Bai Hassan oil well -25, Kirkuk area central northern part of Iraq. Baba Formation is subdivided into three microfacies, which are: Fine to very coarse larger Foraminifera packstone, Fine bioclastic smaller Foraminiferal packstone and Fine bioclastic smaller Foraminiferal wackestone. The depositional environment of Oligocene Carbonate may be a part of an attached platform area, where more or less open marine prevailed through out.
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