东天山柴窝堡铜矿成矿构造系列与远景评估  

METALLOTECTONIC SERIES AND PROSPECTIVE EVOLUATION OF CHAIWOBAO COPPER DEPOSITS IN EAST TIANSHAN MOUNTAIN

作　　者：汪劲草[1] 王建业[2] 王正云 彭恩生[1] 

机构地区：[1]中南工业大学,长沙410083 [2]有色金属工业总公司矿产地质研究院,桂林541004

出　　处：《地质与勘探》2000年第5期24-26,共3页Geology and Exploration

基　　金：国家自然科学基金项目!(编号 :49772 15 2 );中国有色金属工业总公司科研项目

摘　　要：柴窝堡铜矿区的层状铜矿属层间水压角砾岩控制的铜矿 ,脉状铜矿属高角度水力断裂控制的铜矿。首次在杏树沟发现产于石英钠长斑岩脉中的铜矿 ,并鉴别出铜沟控制Ⅰ号矿体的成矿构造为热泉通道。上述 4类成矿构造分属岩浆成矿构造系列与水压成矿构造系列。建立的成矿构造模式表明深部具有很好的找铜前景。The layer copper deposit is a kind of copper deposit controlled by interlayer hydrofracturing classtic rock, and vein copper deposit is a kind of copper deposit controlled by high-angle hydrofracturing faults in Chaiwobao copper deposits. Author has first discovered a new type of copper deposit formed in imandrite porphyry vein in Xingshugou, and distinguished that the metallotectonics, which controlls No.I orebody in Tonggou, is the passway of hot spring. The four metallotectonic types above are divided into metallotectonic series of magmatism and metallotectonic series of hydrofractaring respectively, and the metallotectonic model in this paper indicates that Chaiwobao deposits has a excellent ore-hunting future in depth.

关 键 词：成矿构造 成矿构造系列 铜矿床 远景评估 

分 类 号：P618.41[天文地球—矿床学]