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赣中变质岩带的岩石学特征及原岩恢复
引用本文:胡恭任,刘丛强,章邦桐,于瑞莲. 赣中变质岩带的岩石学特征及原岩恢复[J]. 江西地质, 1999, 13(3): 163-167
作者姓名:胡恭任  刘丛强  章邦桐  于瑞莲
作者单位:1. 中国科学院地球化学研究所,贵州,贵阳,550002
2. 南京大学地球科学系,江苏,南京,210093
3. 华侨大学环境保护研究所,福建,泉州,362100
基金项目:国家杰出青年科学基金!(49625304),华侨大学科研起动资金资助项目
摘    要:野外地质调查和详细的岩性岩相学及构造学研究表明,赣中变质岩带由深层次结晶基底和浅层次褶皱基底组成。结晶基底中除斜长角内岩为正变质岩体,其它变质岩均为副变质,斜长角闪岩原岩为基性火成岩,副变质岩原岩主要为杂砂岩,其次为长石砂岩,岩屑砂岩,粘土岩,褶皱基底其原岩为泥质岩,含炭泥质岩(炭质)硅质岩。

关 键 词:变质岩  原岩恢复  江西中部

PETROLOGICAL FEATURES OF THE CENTRAL JIANGXI METAMORPHIC BELT AND RESTORATION OF PROTOLITH
HU Gong-ren,LIU Cong-qiang,ZHANG Bang-tong,YU Rui-lian. PETROLOGICAL FEATURES OF THE CENTRAL JIANGXI METAMORPHIC BELT AND RESTORATION OF PROTOLITH[J]. Jiangxi Geology, 1999, 13(3): 163-167
Authors:HU Gong-ren  LIU Cong-qiang  ZHANG Bang-tong  YU Rui-lian
Abstract:Field geological survey and detailed lithologic-lithofacies and structural study have revealed that the Central Jiangxi Metamorphic Belt is composed of deep-seated crystalline basement and shallow-seated folded basement.In the crystalline basement,the protolith of amphibolite(an ortho-metamorphic rock)is a basic igneous rock,while that of other metamorphic rocks(a para-metamorphic rock)is largely a graywacke with minor arkose,lithic sandstone and clay rock.In the folded basement,the protoliths are pelitic rocks,carbonaceous pelitic rocks and(carbonaceous)siliceous rocks.
Keywords:metamorphic rock  restoration of protolith  Central Jiangxi
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