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1、1000-0569/2014/030(02)-0401-14ActaPetrologicaSinica巖石學(xué)報(bào)*南秦嶺山陽(yáng)-柞水礦集區(qū)構(gòu)造-巖漿-成礦作用1223456閆臻王宗起陳雷劉樹(shù)文任濤徐學(xué)義王瑞廷1223456YANZhen，WANGZongQi，CHENLei，LIUShuWen，ＲENTao，XUXueYiandWANGＲuiTing1.中國(guó)地質(zhì)科學(xué)院地質(zhì)研究所，大陸構(gòu)造與動(dòng)力學(xué)國(guó)家重點(diǎn)實(shí)驗(yàn)室，北京1000372.中國(guó)地質(zhì)科學(xué)院礦產(chǎn)資源研究所，北京1000373.北京大學(xué)地質(zhì)學(xué)系，北京1008714.西北有色地
2、質(zhì)勘查局七一三總隊(duì)，商洛7260005.西安地質(zhì)礦產(chǎn)研究所，西安7100546.西北有色地質(zhì)勘查局地質(zhì)研究院，西安7100541.StateKeyLaboratoryforContinentalTectonicsandDynamics，InstituteofGeology，ChineseAcademyofGeologicalSciences，Beijing100037，China2.InstituteofMineralＲesources，ChineseAcademyofGeologicalSciences，Beijing1
3、00037，China3.DepartmentofGeology，PekingUniversity，Beijing100871，China4.No.713PartyofNorthwestGeoExplorationBureauforNonferrousMetals，Shangluo726000，China5.Xi’anInstituteofGeologyandMineralＲesources，Xi’an710054，China6.InstituteofGeology，NorthwestGeoExplorationBurea
4、uforNonferrousMetals，Xi’an710054，China2013-05-11收稿，2013-10-11改回.YanZ，WangZQ，ChenL，LiuSW，ＲenT，XuXXandWangＲT.2014.Tectono-magmatismandmetallogenesesofShanyang-ZhashuioreconcentrationareainQinlingOrogen.ActaPetrologicaSinica，30(2):401－414AbstractShanyang-Zhashuioreco
5、ncentrationareaisoneimportantunitoftheQinlingmetallogenicbelt.ItexperiencedoceanicsubductionandcontinentalcollisionduringNeoproterozicandLateJurassic-EarlyCretaceousperiods，whichformeddifferenttypesofmineralizationandoredepositssuchasCu，PbZn，Ag，F(xiàn)e，MoandAuindiffere
6、ntprocessoftectonicevolution.ThetitanomagnetitedepositwhichishostedinthemaficrockswasformedbysubductionofthePaleo-QinlingOceanduringNeoproterozoic.ContinoussubductionofthePaleo-QinlingOceanresultedinformationofShanyang-Zhahuiforearcbasinwhichhostedinsedimentary-ty
7、pedepositsofFe，AgandPbZnduringDevonian-Permian.FromTriassictoLateJurassic-EarlyCretaceous，NorthChinacollidedwithSouthChinaandrelatedmineralizationalsoformedduringthisprocess，buttheTriassicporphyry-skarntypeofModepositsandorogenictypeofAudepositsformedinthecollisio
8、nalenvironmentandLateJurassic-EarlyCretaceousporphyry-skarntypeofCuMo-Audepositsformedinapost-collisionalextensiveenvironment.Thesefactsindicatethatthes
