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dc.contributor.authorAlgibouri, Amer S.-
dc.date.accessioned2022-10-18T07:55:00Z-
dc.date.available2022-10-18T07:55:00Z-
dc.date.issued2013-
dc.identifier.urihttp://localhost:8080/xmlui/handle/123456789/2725-
dc.description.abstractThe Lower Jurassic Silisiclastic – Carbonate Succession of Western Iraq is represented by Ubaid, Hussinyiat and Amij formations. It was subdivided into several microfacies that are distinguished on the basis of their depositional texture. Five distinct depositional setting were recognized: fluvial, restricted marine, shallow open marine, inner barrier and Shoal. Based on microfacies and sequence stratigraphic study, five third order sequences in K.H.5/4 were identified. These cycles were divided into eight asymmetrical fourth orders, their asymmetry reflect the imbalance between the rate of sea level fluctuations and rate of subsidence and low sediment influx.en_US
dc.publisherJ. of university of anbar for pure scienceen_US
dc.subjectSequence Stratigraphyen_US
dc.subjectLower Jurassic Formationsen_US
dc.subjectKey Hole, 5/4en_US
dc.subjectWestern Iraqen_US
dc.titleSequence Stratigraphy of the Lower Jurassic Formations in Key Hole, 5/4 - Western Iraqen_US
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