紫苏花岗岩

研究区内广泛出露的太古代岩石属于迁西群麻粒岩，包括麻粒岩、紫苏花岗岩、辉石-斜长片麻岩、角闪岩等。

The Archaean rocks widely exposed in the area studied belong to the Qian-xi Group of granulite facies , including granulite , charnockite , pyroxene ( and / or amphibole ) - plagioclase gneiss , amphibolite and so on .

无论是缺乏流体（脱水熔融）还是存在流体（富CO2）的热作用都表明，从地壳岩石形成紫苏花岗岩需要低H2O环境。

Both fluid-absent ( dehydration melting ) and fluid-present ( rich in CO_2 ) heating show the charnockites formed from the crustal rocks require lower-H_2O environment .

矿物组成、结构和野外产状表明：这些紫苏花岗岩是火成成因的。

Mineral assemblage , texture and field occurrence indicate an igneous origin for the charnockites .

综述了麻粒岩、紫苏花岗岩和混合岩中流体包裹体研究进展；

The research progress of fluid inclusions in granulites , charnockites and migmatites is reviewed in this paper .

琼中地区存在由片麻岩、混合岩、麻粒岩和紫苏花岗岩组成的高级变质杂岩。

The high grade metamorphic complexes in middle Hainan Island are composed of gneisses , migmatites , granulites and charnockites .

山东沂水紫苏花岗岩中残晶相矿物的发现及紫苏花岗岩的形成过程弯晶的沟道效应

Occurrence of the restite minerals in CHARNOCKITES and the processes of charnockite formation in Yishui area , shandong province channeling effects in bent crystal

广西大容山&十万大山岩带紫苏辉石董青石花岗岩套矿物学研究

Study mineralogy of hypersthene cordierite granite suite along darongshan - shiwandashan rock zone in Guangxi