چکیده

Lower Cretaceous strata in Kopet-Dagh basin (Iran Turkmenistan and Afghanistan) have hydrocarbon potential and are mostly composed of medium- to thick-bedded mostly grainy limestones with various skeletal (bivalves foraminifera algae echinoderms brachiopods) 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 sequense 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. According to the study conducted from the west of the basin to the east and Afghanistan the thickness of carbonate deposits and reservoir potential decreases. 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.

کليدواژه ها

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

کد مقاله / لینک ثابت به این مقاله

برای لینک دهی به این مقاله، می توانید از لینک زیر استفاده نمایید. این لینک همیشه ثابت است :

نحوه استناد به مقاله

در صورتی که می خواهید در اثر پژوهشی خود به این مقاله ارجاع دهید، به سادگی می توانید از عبارت زیر در بخش منابع و مراجع استفاده نمایید:
شیرین فرهادمهر , 1402 , بررسی رخساره های رسوبی و چینه نگاری توالی در یکی از مخازن احتمالی هیدروکربنی حوضه کپه داغ، شمال شرق ایران (سازند تیرگان) , هفتمين همايش ملي انجمن رسوب شناسي ايران