江西中南部中新元古代—晚三叠世岩石谱系单位划分  

The Division of Hierarchical Units of Intrusive Rocks from Middle-late Proterozoic to Late Triassic in Middle-south Jiangxi Province

作　　者：刘春根 刘邦秀 李永明 聂高安 

机构地区：[1]江西省地质调查院,江西向塘330201

出　　处：《华东地质学院学报》2002年第3期195-198,共4页Journal of East China Geological Institute

摘　　要：依据不同构造岩浆区单元 ,江西中南部中新元古代 -晚三叠世的侵入岩可划分为武夷山构造岩浆区、赣西南构造岩浆区。其中武夷山构造岩浆区共划分了 43个单元 ,归并为 11个超单元 ;赣西南构造岩浆区共划分为 34个单元 ,归并为10个超单元。这样较系统地建立了江西省中南部中新元古代 -晚三叠世岩石谱系单位和等级体制 ,为今后开展全省侵入岩谱系单位划分奠定了基础。The intrusive rocks from middle-late proterozoic to late triassic in middle-south Jiangxi privince can be divided into two tectonic-magma areas of Wuyishan and south-west Jiangxi. The intrusive rocks in the tectonic-magma area of Wuyishan is divided into 43 units and incorporated into 11 super-units, and the intrusive rocks in south-west is divided into 34 units and incorporated into 10 super-units. It laid the foundations of the division of hierarchical units of intrusive rocks in Jiangxi province.

关 键 词：岩石谱系单位 侵入岩 中新元古代 晚三叠世 江西 

分 类 号：P534[天文地球—古生物学与地层学] P588.12[天文地球—地质学]