Qualitative and quantitative study of the microfacies of the Sarvak Formation Kuh-e Khane-Kat and Kuh-e Shah-Neshin Sections in Fars province
(ندگان)پدیدآور
Afghah, MasihDehghanian, Mohammadsadegنوع مدرک
TextOriginal Article
زبان مدرک
Englishچکیده
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.
کلید واژگان
Sarvak Formationmicrofacies
Fars
Khane-Kat mountain
Shah-Neshin mountain
شماره نشریه
1تاریخ نشر
2007-03-011385-12-10
ناشر
Islamic Azad University, Zahedan Branchسازمان پدید آورنده
Department of Geology, Islamic Azad University - Shiraz Branch, Shiraz, IranDepartment of Geology, Islamic Azad University - Shiraz Branch, Shiraz, Iran
شاپا
1735-85662383-0883




