Microfacies and Sedimentary Environments of Dalan Formation at Surmeh Mountain, Folded Zagros Zone, Southwestern Iran
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چکیده
منابع مشابه
Sedimentary Facies, Architectural Elements and Trace Fossils of Kashkan Formation, Folded Zagros Zone in SW Iran
The Kashkan Formation (Paleocene to Middle Eocene), consists of conglomerate, sandstone, and siltstone in the Zagros Folded zone, southwest Iran. Type of the sedimentary facies, architectural elements and trace fossils show that Kashkan deposits were formed in a low sinuosity braided stream system, with north to south flow direction. The formation displays coarsening-upward succession reflects ...
متن کاملsedimentary facies, architectural elements and trace fossils of kashkan formation, folded zagros zone in sw iran
the kashkan formation (paleocene to middle eocene), consists of conglomerate, sandstone, and siltstone in the zagros folded zone, southwest iran. type of the sedimentary facies, architectural elements and trace fossils show that kashkan deposits were formed in a low sinuosity braided stream system, with north to south flow direction. the formation displays coarsening-upward succession reflects ...
متن کاملFolding Geometry Surveys of Asef Mountain, Northern Shiraz (Southwestern Folded Zagros Belt)
In this paper the geometrical relationship of the folds which exist in the Folded Zagros Mountains, including Asef Mountain (northern Iran), were studied. The southern and western zones of the Zagros Mountains are called the Folded Zagros. These zones extend approximately 1,375 km in length with a width ranging from 120 to 250 km. Asef Mountain is located in northern Shiraz (from northern Sarda...
متن کاملLithofacies and Sedimentary Environments of Aghajari Formation in Dehsheikh Mountain, West of Shiraz, Iran
Aghajari Formation, known as Upper Fars Group, is developed throughout the Folded Zagros Zone and has a thickness of 2966 m in its type section in SW of Iran and 1473 m in the study area, located 20 km west of Shiraz. Aghajari Formation, in this area, consists of three major facies associations. These are "fine", "medium" and "coarse" grained terrigenous sediments, usually interpreted as channe...
متن کاملFirst Finding of Satin Spar Gemstone in Iran, Folded Zagros Zone, Fars Region
The gypsum mineralization occurred in the form of Satin Spar and Selenite in the south and southwest of the Fars province in the folded Zagros zone. In this region, Satin Spar mineralization has been formed as stratiform between the red marl and siltstone units of Late Miocene–Pliocene in Agha Jari, Bakhtiari, and the Gachsaran formations. The reserves of Satin Spar in this area are at least 20...
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ژورنال
عنوان ژورنال: International Journal of Basic and Applied Sciences
سال: 2012
ISSN: 2227-5053
DOI: 10.14419/ijbas.v1i4.251