Al-Ehmeedy, , Safwan, , Lihaibi, A., A. Al-Miamary, F. (2012). Microfacies Analysis and facies model of Khurmala Formation (U.Paleocene – L. Eocene), Dokan Area, northeastern Iraq.. , 17(3), 186-195.
Al-Ehmeedy; Safwan; AL- Lihaibi; Falah A. Al-Miamary. "Microfacies Analysis and facies model of Khurmala Formation (U.Paleocene – L. Eocene), Dokan Area, northeastern Iraq.". , 17, 3, 2012, 186-195.
Al-Ehmeedy, , Safwan, , Lihaibi, A., A. Al-Miamary, F. (2012). 'Microfacies Analysis and facies model of Khurmala Formation (U.Paleocene – L. Eocene), Dokan Area, northeastern Iraq.', , 17(3), pp. 186-195.
Al-Ehmeedy, , Safwan, , Lihaibi, A., A. Al-Miamary, F. Microfacies Analysis and facies model of Khurmala Formation (U.Paleocene – L. Eocene), Dokan Area, northeastern Iraq.. , 2012; 17(3): 186-195.

Microfacies Analysis and facies model of Khurmala Formation (U.Paleocene – L. Eocene), Dokan Area, northeastern Iraq.

Tikrit Journal of Pure Science
Article 1, Volume 17, Issue 3, 2012, Pages 186-195
Authors
; ; AL- Lihaibi; Falah A. Al-Miamary
Abstract
The present study include micofacies analysis of Khurmala Formation(U.Paleocene – L. Eocene), Dokan Area, northeastern Iraq.The Formation units is divided to five main microfacies which divided to (11) Sub- microfacies (Dolomitized Lime Mudstone, Bioclastic Lime Mudstone, Bioclastic Lime Wackestone, Algal Lime Wackestone, Miliolid Lime Wackestone, Algal Miliolidal Lime Packestone, Algal Lime Packestone, Miliolid Lime Grainstone,Algal Miliolid Lime Grainstone, Peloidal Lime Grainstone, Boundstone microfacies) . The micofacies indicated that the Formation has deposited in a semi_ restricted quiet Lagoon , reef mound and tidal flat (intertidal).
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