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机构地区:[1]西北有色地质勘查局711总队,陕西汉中723000 [2]成都理工大学,四川成都723000
出 处:《甘肃冶金》2014年第6期92-96,共5页Gansu Metallurgy
基 金:中国地质调查局项目<青海省泽库县萨卡拉卡地区1:5万I47E004021等五幅区域地质矿产调查>(项目编号:1212011221140)
摘 要:尼马龙卡地区位于泽库弧后前陆盆地,区内晚三叠世花岗闪长岩与古浪提组接触带具备热液型金、钨矿成矿地质条件。近年来通过在该区开展1:5万区域地质矿产调查工作,发现了多个化探异常,在水系沉积物异常中心通过1:1万土壤地球化学测量进一步圈定了化探异常。W、Bi、Mo、Au、Ag、As等化探异常明显,元素相关性好,通过对重点化探异常进行验证,发现了较好的找矿线索。土壤地球化学异常中心及北东向构造破碎带具有较大的找矿潜力。Nimalongka area is located in Zeku back-arc foreland basin. The contract zone of the late Triassic granodiorite and Gulangti group has ore-forming geological factors of the epithermal gold deposit and tungsten ore. In recent years,several geochemical anomalies were found by carrying out regional geological and mineral resources survey at 1: 50000 in this area. Further geochemical anomalies through 1: 10000 pedogeochemical anomalies were found in the center of stream sediment anomaly. W,Bi,Au,Ag,As and other geochemical anomalies are obvious and the correlation of these elements is very good. A better clue of prospecting by verifying key geochemical anomalies have been found. The center of pedogeochemical anomalies and the NE-trending tectonic fracture zone have a large exploration potential.
分 类 号:P622.3[天文地球—地质矿产勘探]
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