双井子铁铜矿地质特征及找矿远景分析

摘要

The Shuangjingzi iron-copper deposit is located in Mazhuangshan arc basin in northeast margin of the Tarim plate.The mineralized bodies occurred in marble and granodiorite contact zone, mainly due to the northeast trend struct control, with hydrothermal and skarn rock type mineralization characteristics.%双井子铁铜矿位于塔里木板块东北缘马庄山弧后盆地,矿化体产于大理岩与花岗闪长岩接触带中,主要受北东向构造控制,具有热液型及矽卡岩型成矿特征.