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作 者:王宝金[1] 迟效国[1] 白晶哲[2] 刘忠[3] 徐人愉 袁平[3] 于喜文[3]
机构地区:[1]吉林大学地球科学学院,长春130061 [2]吉林省黄金管理局,长春130021 [3]吉林省地质调查院,长春130061
出 处:《吉林大学学报(地球科学版)》2008年第4期553-558,共6页Journal of Jilin University:Earth Science Edition
基 金:中国地质调查局地质调查项目(20001020052003;200310200029)
摘 要:新疆东昆仑成矿带是我国地质工作程度较低的地区之一,在近年矿产勘查中发现了白干湖钨锡矿床等矿床(点)47处,圈定1∶5(10)万水系沉积物异常114处,并确立了该区属钨的地球化学块体。在成矿地质背景分析的基础上,对白干湖钨锡矿床、喀拉曲哈铜矿床和克孜勒金矿床等典型矿床特征进行了讨论,对区域找矿潜力和白干湖钨锡矿床的找矿潜力进行了分析。结果表明,该成矿带钨锡金铜等矿产找矿潜力巨大,并将成矿带划分为4处成矿远景区和18处成矿预测区。白干湖钨锡矿床有望成为超大型矿床。The degree of geological research in the eastern Kunlun metallogenetic belt, Xinjiang is very low. However, 47 deposits (occurrences), including the Baiganhu W - Sn deposit, and 114 geochemical anomalies in scale 1 : 50000 have been found recent years through varied mineral assessments in the area. It is concluded that the area belongs to a geochemical block of W. Based on the analysis of the geological setting of the area, the geological features of the Baiganhu W - Sn, Kalaquha Cu and Kezile Au deposits were studied, the prospecting potential of the mineral resources of the area and of the Baiganhu W - Sn deposit are discussed. It is suggested that the W - Sn potential of the area is great. Four metallogenetic prospects and 18 potential metallogenetic tracts are defined in the area. The Baiganhu W - Sn deposit should be superlarge.
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