Qualitative and quantitative study of the microfacies of the Sarvak Formation Kuh-e Khane-Kat and Kuh-e Shah-Neshin Sections in Fars province
الموضوعات :Masih Afghah 1 , Mohammadsadeg Dehghanian 2
1 - Department of Geology, Islamic Azad University - Shiraz Branch, Shiraz, Iran
2 - Department of Geology, Islamic Azad University - Shiraz Branch, Shiraz, Iran
الکلمات المفتاحية: Fars, microfacies, Sarvak Formation, Khane-Kat mountain, Shah-Neshin mountain,
ملخص المقالة :
This study is about two stratigraphic sections of the Sarvak Formation, namely Kuh-e Khane-Kat and Kuh-e Shah-Neshin sections. Over 250 meters of the Sarvak Formation and 200 thin sections have been studied. Index microfacies and foraminifers have been identified. Index microfacies include: mudstone, wackestone, packstone and grainstone. The amount of bioclasts have been determined as larger than of the other microfacies elements. Based on micropaleontological data, the age of the Sarvak Formation is Cenomanian.
