新疆索尔库都克铜钼矿床控矿因素及成因探讨  

Ore-Controlling Factors and Genesis Discussion of Cu-Mo Deposit in Suoerkuduke, Xinjiang

作　　者：曹崇林 CAO Chong-lin(Baiyin Institute of Miner Exploration of Gansu Nonferrous Metal Exploration Bureau, Baiyin 730900, China)

机构地区：[1]甘肃省有色金属地质勘查局白银矿产勘查院

出　　处：《甘肃冶金》2019年第3期103-105,共3页Gansu Metallurgy

摘　　要：索尔库都克铜钼矿与火山岩有密切的关系,该矿床既具有接触交代矽卡岩型矿床的特征,也具备火山岩热液矿床的特点,矿床既不同于典型矽卡岩矿床,也不同于非矽卡岩化火山热液矿床,是在特定的地质和成矿条件下形成的,具有其独特性与复杂性。Cu-Mo deposit in suoerkuduke has closed relationship with volcanic rocks, ore deposit has the characteristics of contact metasomatism skarn type deposit, also have the characteristics of volcanic hydrothermal deposit, the deposit is different from skarn deposit, it is also different from the silicon card lithiGcation volcanic hydrothermal deposit, it is formed in the specific geological and metallogenic conditions, it has uniqueness and complexity characteristics.

关 键 词：索尔库都克 铜钼矿床 控矿因素 成因探讨 

分 类 号：P618.41[天文地球—矿床学] P618.65[天文地球—地质学]