摘要
新疆西南天山川乌鲁铜、金、锑多金属矿位于塔里木板块北缘活动带.矿体环绕科克莫依纳克岩株内外接触带分布,严格受接触带控制,同时受围岩图尤克阿秀组和次级构造节理、裂隙的控制,其成矿物质来源于图尤克阿秀组和科克莫依纳克岩株.岩浆侵入活动是该矿成矿物质置换萃取和矿液运移的热动力来源.该矿床成因类型为接触交代-夕卡岩型.
The Chuanwulu copper, gold, antimony polymetallic ore in the southwest Tianshan Mountains of Xinjiang locates in the northern margin mobile belt of the Tarim plate .Orebodies distribute around the Kekemoyinake stocks within and outside the contact zone and be controlled strictly by it as well as by country rock stratum Tuyoukeaxiu group and sub-structural joints, crack, Mineralized sources are from Tuyoukeaxiu group and Kekemoyinake stocks. Magma Intrusion activities are thermal power sources for the mine minerals extraction and mine fluid migration. The genetic type of this deposit is the contact-skam.
出处
《新疆地质》
CAS
CSCD
2007年第4期379-383,共5页
Xinjiang Geology
基金
新疆阿合奇县托什干河上游一带1:5万区域地质矿产调查项目(XJQDW2003-17)资助
关键词
西南天山
多金属矿
地质特征
成矿规律
找矿标志
Polymetallic ore
Geological feature
Ore-forming law
Ore prospecting indicator
The southwest Tianshan mountains
