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江西北武夷山高家山铜钼矿含矿岩体的特征与锆石U-Pb年代学研究
引用本文:曹圣华,唐峰林,黄新曙,邱文江,袁振国.江西北武夷山高家山铜钼矿含矿岩体的特征与锆石U-Pb年代学研究[J].地质学报,2011,85(2).
作者姓名:曹圣华  唐峰林  黄新曙  邱文江  袁振国
作者单位:曹圣华,CAO Shenghua(中国地质大学地球科学与资源学院,北京,100083;江西省地质调查研究院,南昌,330030);唐峰林,黄新曙,邱文江,袁振国,TANG Fenglin,HUANG Xinshu,QIU Wenjiang,YUAN Zhenguo(江西省地质调查研究院,南昌,330030)
基金项目:中国地质调查局"全国重要矿产和区域成矿规律研究","江西铅山-永平地区矿产资源远景调查"(编号1212010881403)资助的成果
摘    要:北武夷山地区高家山矽卡岩型铜钼多金属矿床位于扬子地块与华夏地块碰撞对接带萍乡-广丰深大断裂的甫侧,前人获得与成矿有关正长斑岩、花岗斑岩体的K-Ar法同位素年龄为63.6 Ma、84.7 Ma.本文对与成矿有关的正长斑岩和侵入于正长斑岩、花岗斑岩中的闪长玢岩分别进行了精确的锆石U-Pb定年研究,获得锆石206Pb/238U年龄分别为232.7±0.6 Ma和219.6±1.5 Ma,属印支期.通过分析矿石的氧、硫同位素和成矿岩体的地质地球化学特点,认为高家山铜钼矿床与印支期富碱性岩浆活动存在密切的时空和成因联系.因此,成矿岩体年龄间接地反映了本矿床的形成时代为印支期,提供了北武夷山地区印支期成矿作用的新信息.

关 键 词:锆石U-Pb定年  成矿岩体  高家山  北武夷山

Characteristics and Zircon U-Pb Geochronology of Metallogenic Granitoids in the Gaojiashan Cu-Mo Deposits,Northern Wuyishan,Jiangxi Province
CAO Shenghua,TANG Fenglin,HUANG Xinshu,QIU Wenjiang,YUAN Zhenguo.Characteristics and Zircon U-Pb Geochronology of Metallogenic Granitoids in the Gaojiashan Cu-Mo Deposits,Northern Wuyishan,Jiangxi Province[J].Acta Geologica Sinica,2011,85(2).
Authors:CAO Shenghua  TANG Fenglin  HUANG Xinshu  QIU Wenjiang  YUAN Zhenguo
Affiliation:CAO Shenghua1,2),TANG Fenglin2),HUANG Xinshu2),QIU Wenjiang2),YUAN Zhenguo2)1)Faculty of Earth Science and Resource,China University of Geosciences,Beijing,100083,2)Geological Survey of Jiangxi Province,Nanchang,330030
Abstract:Gaojiashan copper and molybdenum deposits in the northern Wuyi Shan region,Jiangxi province,is tectonically located on the southern margin of the Pingxiang-Gangfeng fault belt,the collisional suture between Yantze plateform to the north and Huaxia plateform to the south.The K-Ar dating ages by previous studies for orthophyre and granite porphyry related to mineralization are 63.6 Ma and 84.7 Ma,respectively.Precise zircon U-Pb dating was carried out on the orthophyre,and diorite porphyry intruding orthophyr...
Keywords:zircon U-Pb dating  metallogenic granitoids  Gaojiashan  northern Wuyi Shan  
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