Aziz Mahmmod AL - Hamdani, A., Jmaad Al - Taayi, A. (2008). Facies and Depositional Environment of Serigakni Formation at Sinjar Structure – Northwest Iraq. , 26(1), 67-79.
Abdul Aziz Mahmmod AL - Hamdani; Ammar Jmaad Al - Taayi. "Facies and Depositional Environment of Serigakni Formation at Sinjar Structure – Northwest Iraq". , 26, 1, 2008, 67-79.
Aziz Mahmmod AL - Hamdani, A., Jmaad Al - Taayi, A. (2008). 'Facies and Depositional Environment of Serigakni Formation at Sinjar Structure – Northwest Iraq', , 26(1), pp. 67-79.
Aziz Mahmmod AL - Hamdani, A., Jmaad Al - Taayi, A. Facies and Depositional Environment of Serigakni Formation at Sinjar Structure – Northwest Iraq. , 2008; 26(1): 67-79.

Facies and Depositional Environment of Serigakni Formation at Sinjar Structure – Northwest Iraq

basrah journal of science
Article 1, Volume 26, Issue 1, 2008, Pages 67-79    PDF (0 K)
Authors
Abdul Aziz Mahmmod AL - Hamdani; Ammar Jmaad Al - Taayi
Abstract
The facies analysis of Serigakni Formation carbonates (Late Oligocene - Early Miocene), which has been studied across two surface sections (Bara and Jaddala) in Sinjar structure, showed that the succession is composed of the alternation of eight Globigerinal mud supported microfacies. This analysis revealed that the most Serigakni succession might be deposited in deep shelf margin zone and occasionally basin zone. Although, since the beginning of it’s middle unit at Bara section and upper unit at Jaddala section, the succession affected by abrupt intermittent low density turbidity current
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