| 赵德怀,华北,庞波,吴浩,梁东,祁斌年.新疆伽师铜矿床地质-地球化学特征及矿床成因[J].地质找矿论丛,2022,37(3):316-326 |
| 新疆伽师铜矿床地质-地球化学特征及矿床成因 |
| Gecological and geochemical characteristics and genesis of Jiashi Cu deposit in Xinjiang |
| 投稿时间：2022-03-15 |
| DOI：10.6053/j.issn.1001-1412.2022.03.007 |
| 中文关键词: 伽师铜矿 矿床地质特征 岩石地球化学特征 物源区构造环境 沉积层控砂岩型 新疆 |
| 英文关键词:Geological characteristics of the Cu deposit petro geochemical characteristics tectonic environment of source area sedimentary stratobound sandstone-hosted Cu deposit Xinjiang |
| 基金项目:招金矿业股份有限公司科研项目"新疆伽师县铜辉矿业有限责任公司勘探区砂岩型铜矿成矿模式及找矿靶区预测"资助。 |
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| 中文摘要: |
| 新疆伽师铜矿床产于新生界古近系苏维依组中，通过对新疆伽师铜矿床地质特征、赋矿的苏维依组岩石化学、微量元素和稀土元素地球化学特征研究表明，伽师铜矿区富集Pb、Cu、Ag、As元素，具有较好的铜成矿背景；赋矿的古近系苏维依组的物源区构造环境为活动大陆边缘；Cu元素主要来自于上白垩统巴什基奇克组的风化产物；铜矿床的形成明显受地层、岩性、古气候环境和构造的控制，属古近系潟湖相沉积作用和构造富集作用有关的砂岩型沉积-构造富集型铜矿床。 |
| 英文摘要: |
| Jiashi Cu deposit occurs in Suweiyi formation of Cenozoic Palaeogene System. The geological characteristics of the deposit and research on geochemistry, trace element and REE geochemistry of the host rock of Suweiyi formation show that the surrounding area of the deposit is riched in Pb, Cu, Ag, As with potential for Cu ore prospecting. Source area of Suweiyi formation is active continental margin. Cu comes mainly from the weathered material of Upper Cretaceous Bashijiqike formation. The Cu deposit is apparently controlled by stratum, lithology, palaeo-climate and tectonics. It is a sandstone-hosted sedimentary-tectonic ore material enriched Cu deposit related to lagoon sedimentation. |
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