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江西九(江)瑞(昌)地区花岗岩类的演化及其控矿作用
引用本文:崔彬.江西九(江)瑞(昌)地区花岗岩类的演化及其控矿作用[J].现代地质,1993,7(3):337-345.
作者姓名:崔彬
作者单位:中国地质大学 北京
摘    要:江西九(江)瑞(昌)铜金矿田是长江中下游铁、铜、金成矿带的重要组成部分。受环太平洋共振构造带的影响,区内燕山期岩浆活动频繁,形成近30个浅—超浅成中酸性侵入体,主要含矿岩体从早至晚沿石英闪长玢岩→花岗闪长斑岩→石英斑岩方向演化,伴随这一演化趋势,岩体的含矿性也发生相应变化:Au→Cu→Mo,它们直接控制了区内铜、金矿床的转化。

关 键 词:九瑞地区  花岗岩类  控矿作用

EVOLUTION AND ORE-CONTROL ACTION OF THE GRANITOIDS IN JIUJIANG-RUICHANG AREA,JIANGXI PROVINCE
Cui Bin.EVOLUTION AND ORE-CONTROL ACTION OF THE GRANITOIDS IN JIUJIANG-RUICHANG AREA,JIANGXI PROVINCE[J].Geoscience——Journal of Graduate School,China University of Geosciences,1993,7(3):337-345.
Authors:Cui Bin
Abstract:Jiujiang-Ruichang ore area of copper and gold is an important part of Fe. Cu and Au met- allogenetic belt in the middle and lower reaches of Yangtze river. Since affected by circum-Pacific resonant tectonic belt, the magmatic activity of Yanshan period took place frequently and brought the forming of about 30 hypabyssal- ultrahy- pabyssal, intermediate- acldic rock bodies. The major ore-bearing rock bodies are of quartz diorite porphyry-granodiorite porphyry-quartz porphyry from early to late time. With the vari- ation of this evolution, the commodity in rock bodies changed relevantly: Au→Cu→Mo
Keywords:Jiujiang-Ruichang area  granitoids  ore-control action  
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