ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
湘东北金鸡金矿床岩体成岩机制
  
关键词:granite  granodiorite  petrogeochemistry  geochronology  Jinji Au deposit  Jiangnan orogenic belt
基金项目:国家重点研发计划“深地资源勘查开采”重点专项课题(编号: 2017YFC0601501);中南大学创新驱动计划(编号: 1053320180985)
作者单位E-mail
隗含涛 中国地质科学院矿产资源研究所, 自然资源部成矿作用与资源评价重点实验室
中南大学地球科学与信息物理学院
中南大学有色金属成矿预测与地质环境监测教育部重点实验室 
csuwht@126.com 
邵拥军 中南大学地球科学与信息物理学院
中南大学有色金属成矿预测与地质环境监测教育部重点实验室 
 
汪程 中南大学地球科学与信息物理学院
中南大学有色金属成矿预测与地质环境监测教育部重点实验室 
 
刘清泉 中南大学地球科学与信息物理学院
中南大学有色金属成矿预测与地质环境监测教育部重点实验室 
 
刘忠法 中南大学地球科学与信息物理学院
中南大学有色金属成矿预测与地质环境监测教育部重点实验室 
 
肖克炎 中国地质科学院矿产资源研究所, 自然资源部成矿作用与资源评价重点实验室  
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摘要:
Petrogenesis of the Granitoids in the Jinji Au Deposit, Northeastern Hunan Province
      The Middle–Early Paleozoic granitoids in Hunan section of the Jiangnan orogenic belt are of great significance for the study of the Early Paleozoic tectonic evolution and gold mineralization. Two types of granitoids, i.e., granite and granodiorite, were recently found in the Jinji gold deposit, which is located in the central section of the orogenic belt. Two types of rock samples were dated by zircon La-ICPMS U-Pb technique, and the results show that the granite and granodiorite yielded U-Pb zircon ages of (425.2±1.5) Ma and (430.6±1.5) Ma, respectively. The geochemical data showes that the granite belongs to I-type granite, which was derived from partial melting of metapelitic rocks in the crust; the granodiorite belongs to adakite, which was derived from partial melting of metasandy rocks in the crust. The Sr-Nd isotopic analysis shows that the granodiorite has higher (87Sr/86Sr)i values of 0.722 369 and 0.722 488, lower (143Nd/144Nd)i values of 0.511 941 and 0.511 990 and lower εNd(t) values of 8.2 and 7.2, and the two-stage Nd model ages of the granodiorite are 1.75 Ga and 1.84 Ga, which are consistent with the ages of metamorphic basement in the Jiangnan orogenic belt (1.65~2.14 Ga). The petrogeochemical, geochronologic and Sr-Nd isotopic characteristics of granites and granodiorites in the Jinji gold deposit indicate that they were produced by Early Paleozoic intracontinental orogenic events in South China, and the results help to investigate the geodynamic mechanism for Au mineralization in northeastern Hunan Province.
WEI Han-tao,SHAO Yong-jun,WANG Cheng,LIU Qing-quan,LIU Zhong-fa,XIAO Ke-yan.2020.Petrogenesis of the Granitoids in the Jinji Au Deposit, Northeastern Hunan Province[J].Acta Geoscientica Sinica,41(2):253-266.
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