ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
班—怒成矿带西段躬穷左波Fe-Cu矿区侵入岩年代学及地球化学特征
  
关键词:zircon U-Pb dating  whole-rock geochemistry  Gongqiongzuobo  Bangong Co–Nujiang metallogenic belt
基金项目:中国地质调查局地质调查项目(编号: DD20160026);国家自然科学基金项目(编号: 41403040)
作者单位E-mail
旦真王修 中国地质大学(北京)地球科学与资源学院 dzwx@cugb.edu.cn 
王立强 中国地质科学院矿产资源研究所 wlq060301@163.com 
王勇 中国地质大学(北京)地球科学与资源学院  
李志军 成都理工大学地球科学学院  
李申 成都理工大学地球科学学院  
李壮 中国地质科学院矿产资源研究所  
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摘要:
Geochronology and Geochemistry of Main Intrusions of the Gongqiongzuobo Fe-Cu Ore Occurrence in the Western Bangong Co–Nujiang Metallogenic Belt, Tibet and Its Geological Significance
      This paper reports systematic research about LA-ICP-MS zircon U-Pb age, whole-rock major and trace element of three acid intrusives from the Gongqiongzuobo Fe-Cu deposit. The result of Geochronology testing shows that the weighted average age are 147.0 Ma(Granite porphyry), 143.6 Ma(Monzonitic granite porphyry) and 142.8 Ma(K-feldspar granite) respectively and finds there are three periods of magma activity in Gongqiongzuobo area during late jurassic-early cretaceous epoch. The result of geochemistry characteristics shows that (1)Granite porphyry belongs to aluminum-weakly peraluminous I-type granite, (2)Monzonitic granite porphyry is high potassium calc-alkine series and belongs to weakly peraluminous I-type granite, (3)K-feldspar granite has experienced strong crystallization differentiation and belongs to high differentiation I-type granite. Those rocks enrich in Rb Th U Pb and deplete in Nb Ta Ti P, their Nb/Ta ratio are close to continental crust and the zircon has negative εHf(t) value. All these feature implys rock-forming materials are mainly come from the crust-source. The discoveray of late-jurassic skarn-type mineralization has important significance for consummating regional metallogeny and directing regional prospecting.
DANZHEN Wang-xiu,WANG Li-qiang,WANG Yong,LI Zhi-jun,LI Shen,LI Zhuang.2017.Geochronology and Geochemistry of Main Intrusions of the Gongqiongzuobo Fe-Cu Ore Occurrence in the Western Bangong Co–Nujiang Metallogenic Belt, Tibet and Its Geological Significance[J].Acta Geoscientica Sinica,38(5):734-744.
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