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北祁连加里东造山带南缘钨矿成矿背景及找矿潜力
引用本文:林国芳,刘凤萍.北祁连加里东造山带南缘钨矿成矿背景及找矿潜力[J].甘肃地质学报,2003,12(1):78-84.
作者姓名:林国芳  刘凤萍
作者单位:甘肃省有色地质勘查局106队 甘肃兰州730047 (林国芳),甘肃省有色地质勘查局106队 甘肃兰州730047(刘凤萍)
基金项目:中国地质调查局资源调查评价项目 (1 2 1 2 0 1 0 330 6 0 1 )资助
摘    要:北祁连加里东造山带主要钨矿类型为夕卡岩—石英脉型 ,其成矿与加里东中、晚期深源中高侵位中酸性侵入体有成因联系。成矿时代集中于 (4 6 2± 1 3)Ma~ (4 36± 32 )Ma ,与加里东期活动大陆边缘俯冲作用过程中的板块重熔—同熔—岩浆分异作用有关 ,由于其形成于区域大规模火山喷发之后 ,深部岩浆有一定分异 ,并存在广泛的矿源层条件 ,对钨的大规模成矿有利。因此 ,寻找大型以上的钨矿床必须综合考虑岩浆作用和矿源层两个主要因素。锰夕卡岩型银 (铅、锌 )矿床是北祁连南缘寻找大型以上规模钨银多金属矿床的重要目标

关 键 词:夕卡岩—石英脉型  钨矿床  动力学背景  找矿潜力  北祁连

SKARN-QUARTZ VEIN TYPE TUNGSTEN METALLOGENIC SETTING AND PROSPECTING POTENTIAL IN THE SOUTHERN MARGIN OF NORTH QILIAN CALEDONIAN OROGEN NORTHWEST CHINA
LIN Guo,fang and LIU Feng,ping.SKARN-QUARTZ VEIN TYPE TUNGSTEN METALLOGENIC SETTING AND PROSPECTING POTENTIAL IN THE SOUTHERN MARGIN OF NORTH QILIAN CALEDONIAN OROGEN NORTHWEST CHINA[J].Acta Geologica Gansu,2003,12(1):78-84.
Authors:LIN Guo  fang and LIU Feng  ping
Institution:(No.106 Team of Gansu Nonferrous Geological Prospecting Bureau,CNNC,Lanzhou 730047,China)
Abstract:The main W-deposit type in the southern margin of North Qilian Caledonian oro- gen is skarn-quartz vein type which is genetically related to intermediate acid intrusions formed in middle and late Caledonian stage. The main metallogenic age is (462±13)Ma~(436±32) Ma. The W-deposits were formed by oceanic plate re-melting-lower crust syntexis-magma differentiation relating to subduction in the active continental margin in the Caledonian cycle. Be- cause the W-deposits were formed after regional intense volcanic eruption, which means enough time to form differentiated magma, it seems favorable to form large scale tungsten deposi ts. To prospect large tungsten deposits in this area, both factors such as magmatism and W-bearing source beds must be considered together.Another target for Prospecting large Ag(Pb,Zn)deposit is manganoan skarn type.
Keywords:Skarn and quartz vein type  W-deposits  Dynamic setting  Northern Qilian orogen
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