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作 者:赵献丽[1] 秦覃[1] 郭涛[1] 王恒[1] 谭克彬[1] 满毅[1]
机构地区:[1]新疆维吾尔自治区地质矿产勘查开发局第六地质大队,新疆哈密839000
出 处:《中国科技博览》2014年第8期70-72,共3页China Science and Technology Review
摘 要:石门铜金矿位于塔里木板块北山裂谷西段,区域上分布有多处浅成低温热液型金矿床。石门铜金矿自2002年发现至今的近十年内,仅于普查阶段发现一条含铜金蚀变带之后一直没有突破。笔者结合石门铜金矿地质特征,围岩蚀变,矿体特征,对石门铜金矿中的成因矿物学进行了研究,分析矿体赋存部位的地球化学条件,明确了区内有利于金元素沉淀富集的地球化学障的位置,并提出找矿方向及工程布设建议,以期取得找矿突破。Shhnen copper gold deposit is located in the western part of the Tarim plate Beishan Rift Valley,The regional distribution of multiple epithermal gold depositoShimen copper mine two thousand two Found so far in the past ten years,Only in the phase of the census found a after copper bearing gold alteration zone has been no breakthroughoI think Geological characteristics of copper gold deposit in Shimen,country rock alteration^wall-rock alterati, Characteristics of ore body, The genetic mineralogy of Shimen copper gold deposit are studied in, Analysis of the geochemical conditions of ore bodies occur,The area is conducive to the precipitation of gold element geochemical barrier enrichment position, And put forward suggestions for layout of prospecting and Engineering,In order to obtain prospecting breakthrough.
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