Raisi, A. and Lasemi, Y. (2000) Sedimentary Environments Microfacies and Sequence of Asmari Formation (Oligo-Miocene) in South Dezful Embayment. Proceedings of the Fourth Symposium of Geological Society of Iran, Iran, January 2000, 45-53.

has been cited by the following article:

• TITLE: Sequence Stratigraphy and Sedimentary Environment of Sarvak Formation, in the Oil Field of Kuhmond (Southwest of Iran)

  AUTHORS: Jafar Qomi Aveili

  KEYWORDS: Sequence Stratigraphy and Sedimentary Environment, Sarvak Formation, Oil Field of Kuhmond

  JOURNAL NAME: Open Journal of Geology, Vol.6 No.10, October 28, 2016

  ABSTRACT: Sarvak formation is one of the important hydrocarbon reservoirs in the Zagros Basin that is one of the mid-Cretaceous carbonate units in Bangestan group. This formation is located in the Kazhdomi Formation of the slope. Kuhmond oil field is in the southeast of Bushehr and in the north and northwestern of Fars province. In this study, sedimentology studies, stratigraphy and sedimentary environment in Sarvak Formation were studied. Based on studies, 18 main Microfacies were diagnosed in the region that have been deposited in four facies belts including open Sea, dam, lagoon and tidal zones. According to studies, the sedimentary environment of Sarvak formation in Kohmond field was diagnosed as a ramp carbonate platform (Figure 1).