Investigation of sedimentary Facies and sequence Stratigraphy in one of the possible hydrocarbon reservoirs of Kopet-Dagh Basin, NE Iran (Tirgan Formation)

Iranian Journal of Earth Sciences

مقالات آماده انتشار، پذیرفته شده، انتشار آنلاین از تاریخ 30 خرداد 1402

نوع مقاله: Original Research Paper

شناسه دیجیتال (DOI): 10.57647/j.ijes.2024.1603.18

نویسندگان

Shirin Farhadmehr¹؛ Nader Kohansal Ghadimvand¹؛ Mohammad Javanbakht^{* 2}؛ Davood Jahani¹؛ Mohammad Reza Jafari¹

¹Department of Geology, North Tehran Branch, Islamic Azad University, Tehran, Iran

²Department of Geology, Mashhad Branch, Islamic Azad University, Mashhad, Iran

چکیده

Lower Cretaceous strata in Kopet-Dagh basin (Iran, Turkmenistan and Afghanistan) have hydrocarbon potential and are mostly composed of medium- to thick-bedded and nonskeletal (peloids, ooids, and intraclasts) allochems. In this study, two stratigraphic sections in Chaman-Bid and Sorkh-Ghaleh with a thicknesses of 242 and 165 m in NE Iran, have been studied in order to determination of the sedimentary environment and sequence stratigraphy. Based on the field observations, petrographic studies, textural and facies characteristics, as well as the abundance and distribution of foraminifera and other components, 16 carbonate microfacies have been identified. Facies analysis documents low - to high-energy environments, including tidal-flat, lagoonal, shoal, and open-marine facies. Because of the wide lateral distribution of microfacies and the apparent absence of distinct paleobathymetric changes, the depositional system likely represents a westward-deepening homoclinal ramp. Four third-order depositional sequences can be distinguished in each of two stratigraphic sections. Transgressive system tracts (TST) show deepening-upward trends, in which shallow-water (tidal flat and lagoonal) facies are overlain by deeper-water (shoal and open-marine) facies. Highstand systems tracts (HST) show shallowing-upward trends in which deep-water facies are overlain by the shallow facies. All sequence boundaries in the study sections are SB. On the other hand, studies conducted to the north and Turkmenistan show the reservoir potential conditions for these deposits, and since the studies conducted in the study area have similar conditions to the deposits of Turkmenistan, it is hoped that this information can be used to reconstruct the potential. Reservoir in this area to help.

کلیدواژه‌ها

Sedimentary Facies؛ Sequence Stratigraphy؛ Tirgan Formation؛ Kopet-Dagh Zone