赣北钨铜多金属成矿异同性及其与大地构造的成生联系  

Metallogenic Differences and Similarities of a Tungsten-Copper Polymetallic Deposit in Northern Jiangxi Province and Its Genetic Relation with Tectonics

作　　者：陈茂松 刘南庆[2] 秦润君[2] 卢宝荣 CHEN Maosong;LIU Nanqing;QIN Runjun;LU Baorong(Land and Resources Trade Center,Department of Natural Resources of Jiangxi Province,Nanchang 330025,Jiangxi,China;No.916 Geological Party,Jiangxi Bureau of Geology&Mineral Exploration,Jiujiang 332100,Jiangxi,China)

机构地区：[1]江西省自然资源厅国土资源交易中心,江西南昌330025 [2]江西省地质矿产勘查开发局九一六大队,江西九江332100

出　　处：《中国钨业》2020年第2期1-10,共10页China Tungsten Industry

摘　　要：基于赣北地区大陆转换断层及其控岩控矿作用研究成果,侧重从钨铜多金属成矿异同性、大地构造结构与演化及其两者之间的成生联系展开进一步讨论,认为赣北钨铜多金属矿床(田)系区域大地构造演化至燕山期的必然产物,环鄱(鄱阳湖)巨型矿集区乃大陆转换断层作用下古华南洋俯冲带消减—扬子陆块仰冲推覆—壳幔、壳源岩浆生成侵位等系列活动的最终物质存在。Based on the research results of continental transform fault and its rock-controlling and ore-controlling actions in northern Jiangxi,this paper focuses on the similarities and differences of tungsten-copper polymetallic mineralization,tectonic structure and evolution and their genetic relationship.It is believed that the tungsten-copper polymetallic deposit(field)in northern Jiangxi is the inevitable product of regional tectonic evolution to Yanshan period,and the giant ore concentration area around Poyang Lake is the subduction of Nanyang subduction zone in Gu Hua under the action of continental transform fault,the uplift and napping of Yangtze block,and the emplacement of crust mantle and crust magma generation.

关 键 词：成矿异同性 大地构造 成生联系 赣北 

分 类 号：P548[天文地球—构造地质学] TD-05[天文地球—地质学]