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| 西藏墨竹工卡县甲玛铜多金属矿床勘查模型 | |
| 引用本文： | 唐菊兴,邓世林,郑文宝,应立娟,汪雄武,钟康惠,秦志鹏,丁枫,黎枫佶,唐晓倩,钟裕峰,彭慧娟.西藏墨竹工卡县甲玛铜多金属矿床勘查模型[J].矿床地质,2011,30(2):179-196. |
| 作者姓名： | 唐菊兴 邓世林 郑文宝 应立娟 汪雄武 钟康惠 秦志鹏 丁枫 黎枫佶 唐晓倩 钟裕峰 彭慧娟 |
| 作者单位： | 1. 中国地质科学院矿产资源研究所,国土资源部成矿作用与资源评价重点实验室,北京100037 2. 成都理工大学,四川成都,610059 3. 中国石油集团川庆钻探工程有限公司地球物理勘探公司,四川成都,610213 |
| 基金项目： | 本文得到中央公益性行业科研专项“西藏甲玛斑岩铜多金属矿科学基地研究”课题(编号：200911007-02)、国家973项目（编号：2011CB403103）、青藏专项(编号：1212010818089；1212010012005)及中金集团重点勘探项目“E0804”的共同资助 |
| 摘 要： | 甲玛铜多金属矿床是西藏藏中有色金属开发基地的重要矿床.文章重点研究了该矿床的成矿地质条件、找矿标志、地球化学勘查模型、地球物理勘查模型、矿体空间结构等.研究表明:赋矿地层为林布宗组(K1 l)砂板岩、角岩和多底沟组(J3d)大理岩、灰岩,角岩控制了钼(铜)矿体的分布,角岩与大理岩之间的层间构造是矽卡岩型矿体的赋存部位.... |
| 关 键 词： | 地质学 斑岩成矿系统 矿床勘查模型 找矿标志 成矿地质条件 甲玛 西藏 |
An exploration model for Jiama copper polymetallic deposit in Maizhokunggar County, Tibet |
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| TANG JuXing,DENG ShiLin,ZHENG WenBao,YING LiJuan,WANG XiongWu,ZHONG KangHui,QIN ZhiPeng,DING Feng,LI FengJi,TANG XiaoQian,ZHONG YuFeng,PENG HuiJuan.An exploration model for Jiama copper polymetallic deposit in Maizhokunggar County, Tibet[J].Mineral Deposits,2011,30(2):179-196. | |
| Authors: | TANG JuXing DENG ShiLin ZHENG WenBao YING LiJuan WANG XiongWu ZHONG KangHui QIN ZhiPeng DING Feng LI FengJi TANG XiaoQian ZHONG YuFeng PENG HuiJuan |
| Institution: | TANG JuXing1,DENG ShiLin2,ZHENG WenBao2,YING LiJuan1,WANG XiongWu2,ZHONG KangHui2,QIN ZhiPeng2,DING Feng2,LI FengJi3,TANG XiaoQian2,ZHONG YuFeng2 and PENG HuiJuan2(1 MLR Key Laboratory of Metallogeny and Mineral Assessment,Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037,China,2 Chengdu University of Technology,Chengdu 610059,Sichuan,3 Geophysical Exploration Company,Chunqing Drilling Engineering Co.Ltd.,China National Petroleum Corporation,Chengdu 610213,Ch... |
| Abstract: | The Jiama copper polymetallic deposit in Tibet is a significant ore deposit serving as a nonferrous metal base in central Tibet.This paper deals emphatically with the ore bodies in such aspects as its metallogenic geological conditions,prospecting indicators,geochemical exploration model,geophysical exploration model and spatial framework.Studies show that the ore-controlling strata are sandy slate and hornfels of Linbuzong Formation(K1l)and marble and limestone of Duodigou Formation(J3d),and that hornfels ... |
| Keywords: | geology porphyry metallogenic system exploration model of ore deposit prospecting criteria metallogenic geological condition Jiama Tibet |
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