摘要
七宝山铅锌钴矿床地处扬子—华夏古板块结合带七宝山—朱溪深断裂带中部,其矿床成因为沉积后热液叠加改造型,矿床受地层和构造的双重控制~([1])。本文以寻找该类型铜铅锌钴等多金属硫化物矿床为主要目标,通过分析区域成矿构造,区域地球物理化学异常特征,指出七宝山矿区及其周边地区找矿潜力及下步找矿方向。
Qibaoshan lead-zinc-cobalt deposit is located in the middle of the Yangtze-Huaxia paleo-plate assemblage zone Qibaoshan-Zhuxi deep fault zone. The deposit is characterized by the superposition of the hydrothermal superposition and the double control of the strata and the structure~([1]). In this paper, we look for the polymetallic sulfide deposits of this type of copper, lead, zinc and cobalt as the main target, By analyzing the regional metallogenic structure and regional geophysical anomaly, this paper points out the prospecting potential of Qibaoshan mining area and its surrounding area and the prospecting direction.
引文
[1]王学平,周建廷,范爱春.江西省上高县七宝山铅锌铁钴矿床成矿模式[J].东华理工大学学报(自然科学版).2011.27(3).1674-3504.
[2]何细荣,陈国华,刘建光,张诚.江西景德镇朱溪地区铜钨多金属矿找矿方向[J].中国钨业.1009—0622(2011)Ob-0009—06.
[3]余忠珍,罗小洪,丁少辉等.江西北部九岭成矿带锡铜金多金属矿评价成果报告[R].江西省地质调查研究院.2004.12.
[4]江西省地质矿产局.江西省区域地质志[M1]北京:地质出版社,1984.
[5]江西省地质矿产厅.1997.江西省岩石地层[M].武汉:中国地质大学出版社.19-21.
[7]杨明桂,王发宁,曾勇等,著.江西北部金属成矿地质[M].北京:中国大地出版社.2004.
[8]钱国华,赣西铜铅锌矿床类型、地质特征及找矿认识.矿产与地质[J],2003,17,338-341.