松树沟铜矿床地质特征及找矿方向  

GEOLOGICAL CHARACTERISTICS AND EXPLORATION PROSPECTIVITY OF THE SONGSHUGOU COPPER DEPOSIT

作　　者：刘俊涛[1] 杜欣[1] 刘伟[1] 

机构地区：[1]河南省地质调查院

出　　处：《新疆地质》2005年第4期369-372,共4页Xinjiang Geology

基　　金：新疆地矿局1:50000区调招标项目(XJQDZ2003-19)资助

摘　　要：松树沟铜矿矿体主要赋存于二叠纪花岗斑岩体外接触带,明显受花岗斑岩体控制.矿床地球化学特征、矿体特征均显示出斑岩型铜矿床特点.在综合分析松树沟铜矿矿区资料的基础上,探讨矿床成因,提出松树沟铜矿的下步找矿方向,并为西天山地区斑岩型铜矿的找矿方向提供工作思路.The Songshugou copper deposit occurs at the contact of a Permian porphyry granite and is clearly controlled by the porphyry granite. The geochemical and geological characteristics are the same a those of a porphyry copper deposit. A discussion on the genesis of the mineralization is used to determine the next steps for exploration at Songshugou and to guide porphyry copper exploration in west Tianshan region.

关 键 词：讼树沟铜矿 地质特征 找矿方向 

分 类 号：P618.41[天文地球—矿床学]