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四川大宝山铜矿区矿床地质特征及找矿方向
引用本文:毛洪江,梁鲸.四川大宝山铜矿区矿床地质特征及找矿方向[J].沉积与特提斯地质,2008,28(4):82-87.
作者姓名:毛洪江  梁鲸
作者单位:1. 四川省冶金地质勘查局,六○六大队,四川,彭州,611930
2. 四川里伍铜业股份有限公司,四川,九龙,626201
基金项目:四川攀西地区铅锌矿资源调查项目 , 彭县铜矿外围找矿地质调查  
摘    要:层控矿床属火山-沉积变质成因;含铜石英脉型矿床为热液充填成因.根据成矿控制因素和找矿标志,对大宝山地区的成矿远景进行了划分,指出了进一步的找矿方向.

关 键 词:矿床地质特征  矿床类型  找矿方向  大宝山铜矿区

Geology and exploration prospects of the Dabaoshan copper deposit in Pengzhou,Sichuan
MAO Hong-Jiang,LIANG Jing.Geology and exploration prospects of the Dabaoshan copper deposit in Pengzhou,Sichuan[J].Sedimentary Geology and Tethyan Geology,2008,28(4):82-87.
Authors:MAO Hong-Jiang  LIANG Jing
Institution:MAO Hong-Jiang1,LIANG Jing2 (1.No.606 Party,Sichuan Bureau of Metallurgical Geology , Resources Development,Pengzhou 611930,Sichuan,China,2.Liwu Copper Industry Co.,Ltd.,Julong 626201,China)
Abstract:Two types of copper deposits are recognized in the Dabaoshan copper mining district in Pengzhou,Sichuan: stratabound and Cu-bearing quartz vein deposits.The stratabound copper deposit should have a volcanic and sedimentary-metamorphic origin while the Cu-bearing quartz vein copper deposit is of hydrothermal filling origin.The delineation of the exploration prospects has been made on the basis of controlling factors and prospecting criteria.
Keywords:geology  deposit type  exploration prospect  Dabaoshan copper mining district  
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