内蒙古东乌旗巴彦都兰铜矿床地质和地球化学特征及其意义  

Geological and geochemical characteristics of Bayandulan copper deposit,Dong Ujimqin banner,Inner Mongolia and the significance

作　　者：张锋[1] 李志丹[1] 段明[1] 魏佳林 谢瑜[1] 俞礽安[1] 张祺[1] ZHANG Feng LI Zhidan DUAN Ming WEI Jialin XIE Yu YU Reng＇an ZHANG Qi(Tianjin Center of China Geology Survey L a b o r a t o ry of Non - fossil Energy Minerals , Tianjin 300170 , China)

机构地区：[1]中国地质调查局天津地质调查中心非化石能源矿产实验室,天津300170

出　　处：《地质找矿论丛》2017年第2期161-171,共11页Contributions to Geology and Mineral Resources Research

基　　金：地质大调查项目(编号:12120113057400;编号:12120113057300;编号:12120113057100);国家自然科学基金项目(编号:41502082)联合资助

摘　　要：内蒙古巴彦都兰铜矿床位于二连—东乌旗成矿带,该矿区出露下泥盆统泥鳅河组粉砂岩和海西中期黑云母花岗岩体,铜矿体呈脉状产出于泥鳅河组粉砂岩中,严格受断裂控制。主要金属矿物为黄铁矿、磁黄铁矿、黄铜矿等,脉石矿物主要为石英和碳酸盐岩等。矿区黑云母花岗岩La-ICP-MS锆石^(206)Pb/^(238) U加权平均年龄为303.5 Ma±1.1 Ma,铜矿床属于晚古生代构造-岩浆作用的产物。岩石地球化学特征反映黑云母花岗岩属准铝质-弱过铝质高钾钙碱性系列,A/CNK值介于0.99~1.04之间,高碱(w(K_2O+Na_2O)=7.36%~8.73%),富钾(w(K_2O)/w(Na_2O)=1.08~1.66),其形成具有岛弧或后碰撞环境I型花岗岩特征;微量元素特征显示岩体可能形成于后碰撞伸展阶段早期的构造环境中。黄铜矿硫同位素组成介于0.1×10^(-3)~2.1×10^(-3)之间,反映成矿所需的硫可能来自于岩浆,巴彦都兰铜矿区花岗岩很可能是成矿硫的提供者。The Bayandulan copper deposit is located in the Erlian-Dongwuqi metallogenic belt. In the working area are outcropped siltstone of Lower？ Devonian Niqiuhe formation and Middle Hercynian bio- tite granite. Ore bodies occur in the siltstone of Niqiuhe formation and strictly controlled by faults. The main metallic minerals are pyrite, pyrrhotite, chalcopyrite and gangue minerals quartz and carbonatite minerals. Zircons from the biotite granite are analysed for their U-Pb isotopes by La-ICP-MS with the weighted 206 Pb/238 U average age 303. 5 Maztl. 1 Ma, The geochemistry of the rock suggests that the bio- tite granite belongs to metaluminous to weak peraluminous and high k calc alkaline rock series with A/ CNK values from 0. 99 to 1. 04：,high alkali （to （K2 O ＋ Na2 O） = 7. 36% - 8. 73%） and K （ to （K2O）/w （Na2O）=1. 08-1. 66） , characteristic of arc or post-collision I-type granite. Trace element indicated that the granite formed during the early stage of post-collision extension period. The chalcopyrite δ 34 SV-CDT values vary from 0. 1× 10-3 to 2. 1× 10-3 showing that the sulfur is derived from magma. The biotite granite is the most possible supplier of the sulfur thus the copper deposit is the product of Late Paleozoic tectonic-magmatic process.

关 键 词：巴彦都兰铜矿 岩石地球化学 锆石U-PB定年 硫同位素 内蒙古 

分 类 号：P618.41[天文地球—矿床学] P613[天文地球—地质学]