Sedimentary Environment and Sequence Stratigraphy of Fahliyan Formation in Center of Fars
عنوان مقاله: Sedimentary Environment and Sequence Stratigraphy of Fahliyan Formation in Center of Fars
شناسه ملی مقاله: JR_JGEO-5-2_003
منتشر شده در در سال 1388
شناسه ملی مقاله: JR_JGEO-5-2_003
منتشر شده در در سال 1388
مشخصات نویسندگان مقاله:
Alireza Rastegar Lari - Department of Geology, Faculty of Basic Sciences, Islamic Azad University - Sciences and Research Branch, Tehran, Iran
خلاصه مقاله:
Alireza Rastegar Lari - Department of Geology, Faculty of Basic Sciences, Islamic Azad University - Sciences and Research Branch, Tehran, Iran
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).
کلمات کلیدی: Khami Group, Arsenjan, Sivand, Tithonian, Vallanginian
صفحه اختصاصی مقاله و دریافت فایل کامل: https://civilica.com/doc/1320762/