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作 者:秦学文 冯邦国 张云 汪校锋[4] Qin Xuewen;Feng Bangguo;Zhang Yun;Wang Xiaofeng(No.8 Geological Party,Xinjiang Bureau of Geology and Mineral Resources,Aksu,Xinjiang,843000,China;Sichuan Geology and Mineral Bureau Regional Geological Survey Team,Chengdu,Sichuan,610213,China;Tianjin Center of Geological Survey,China Geological Survey,Tianjin,300170,China;Faculty of Computing,China University of Geosciences,Wuhan,Hubei,430074,China)
机构地区:[1]新疆维吾尔自治区地质矿产勘查开发局第八地质大队,新疆阿克苏843000 [2]四川省地质矿产勘查开发局区域地质调查队,四川成都610213 [3]中国地质调查局天津地质调查中心,天津300170 [4]中国地质大学,湖北武汉430074
出 处:《新疆地质》2023年第1期46-50,共5页Xinjiang Geology
基 金:中国地质调查局地质矿产调查项目(1212011120766,DD20160043)资助。
摘 要:研究区位于豫西多金属成矿带,区内发育多处水系沉积物地球化学异常及航磁异常,成矿背景良好。通过1:1万土壤地球化学剖面测量、岩石元素地球化学测量及野外查证,查明该区土壤、岩石元素地球化学背景特征及两者之间的联系,研究成矿元素趋势特征和地球化学异常成因,对1∶20万水系沉积物地球化学异常进行分析与评价,为该区进一步开展矿产评价工作提供可靠依据。The study area is located in Western Henan polymetallic metallogenic belt with good metallogenic back-ground,and several stream sediment geochemical and aeromagnetic anomalies are developed in this area.Through 1:10000 soil geochemical profile survey,and rock element geochemical survey with field verification,the geochemical back-ground characteristics and relationship of soil and rock element were identified,and the trend characteristics of ore-forming elements and the cause of geochemical anomalies were studied.On this basis,the geochemical anomalies of 1:200000 stream sediments were analyzed and evaluated,so as to provide a reliable basis for further mineral evaluation in this area.
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