Sedimentary Environment and Sequence Stratigraphy of Fahliyan Formation in Center of Fars
محل انتشار: دوفصلنامه زمین شناسی ژئوتکنیک، دوره: 5، شماره: 2
سال انتشار: 1388
نوع سند: مقاله ژورنالی
زبان: انگلیسی
مشاهده: 145
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شناسه ملی سند علمی:
JR_JGEO-5-2_003
تاریخ نمایه سازی: 30 آبان 1400
چکیده مقاله:
The Fahliyan Formation (Volgian - Neocomian) (Early Cretaceous) is a part of the Khami Group. This formation has been studied in two sections in the center of Fars (southwest of Arsenjan city and west of Sivand city) to determine its facies, sedimentary environments and sequence stratigraphy. The deposits of the Fahlyian Formation consist of carbonate facies which are deposited in a Carbonate Rimmed Shelf. Two sequences with both type ۱ and type ۲ sequence boundaries are recognized within these deposits which are in accordance with a part of Zuni mega sequence (Lower Zuni III). The age of this formation is referred to the Tithonian- Vallanginian (Early Cretaceous).
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نویسندگان
Alireza Rastegar Lari
Department of Geology, Faculty of Basic Sciences, Islamic Azad University - Sciences and Research Branch, Tehran, Iran