哈密黄土坡铜锌矿地质特征及找矿方法探讨  

GEOLOGICAL CHARACTERISTICS AND PROSPECTING METHODS OF THE HUANGTUPO COPPER-ZINC DOPSIT IN HAMI

作　　者：付明禄 许强奋 曾阳 王福同[3] 

机构地区：[1]新疆西拓矿业有限公司,新疆乌鲁木齐830011 [2]新疆维吾尔自治区有色物探队,新疆乌鲁木齐830011 [3]新疆维吾尔自治区国土资源厅,新疆乌鲁木齐830001

出　　处：《新疆地质》2010年第3期260-266,共7页Xinjiang Geology

摘　　要：哈密铜锌矿是新疆西拓矿业有限公司发现和评价的隐伏中型块状硫化物型铜锌矿床,矿床产于卡拉塔格火山穹窿西南侧下泥盆统卡拉塔格组海相火山岩地层中,黄铁绢英岩(化)是与成矿有关的最重要围岩蚀变,主矿体呈饼状,向NE向侧伏,致密块状构造为主,地球物理特征表现为中-低电阻率,中-高极化率.The Hami cooper-zinc deposit,Insidious medium-sized zinc massive sulfide deposit,It is Discovery and evaluation by Xinjiang Xituo Mining Co.,Ltd.Ore produced in the Lower Devonian Kala Tage Group marine volcanic rocks on the southwest side of the Kala Tage volcanic dome Keywords： Huangtupo;copper-zinc deposit;Geological features;Geophysical characteristics;Pyrite phyllic,the most important ore-related rock alteration is the Pyrite phyllic in this area,The space morphology of main ore body was pie,Side V to the direction of north-east,Compact block structure based,Geophysical characterized by Middle to low resistivity,Middle to high polarizability.

关 键 词：黄土坡 铜锌矿 地质特征 地球物理特征 黄铁绢英岩(化) 

分 类 号：P618.4[天文地球—矿床学]