Petrography and Geochemical Characteristic of Koohrig Intrusive Rocks in Kerman, Iran  

作　　者：Mohammad Baghkhani Mohammad Ali Arian 

机构地区：[1]Department of Geology, Faculty of Science, North Tehran Branch, Islamic Azad University, Tehran, Iran

出　　处：《Open Journal of Geology》2017年第5期683-689,共7页地质学期刊（英文）

摘　　要：Koohrig intrusive mass is located in the east of Rafsanjan, Kerman Province, Iran and it is part of because it has cut the sandstone, limestone, shale units and conglomerate of Upper Cretaceous. Its intrusive rock includes quartz, plagioclase and alkali feldspar and its ferromagnesian mineral which is biotite has changed into chlorite. This Intrusive mass is characterized by the presence of metamorphic geochemical studies led to the detection of granite and granodiorite and quartz monzonite rocks.Koohrig intrusive mass is located in the east of Rafsanjan, Kerman Province, Iran and it is part of because it has cut the sandstone, limestone, shale units and conglomerate of Upper Cretaceous. Its intrusive rock includes quartz, plagioclase and alkali feldspar and its ferromagnesian mineral which is biotite has changed into chlorite. This Intrusive mass is characterized by the presence of metamorphic geochemical studies led to the detection of granite and granodiorite and quartz monzonite rocks.

关 键 词：Urumieh-Dokhtar METAMORPHISM GEOCHEMICAL Studies CALC-ALKALINE Peraluminus Aluminum Saturation Index 

分 类 号：P5[天文地球—地质学]