ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
浅论湘东北地区与燕山期花岗岩有关矿床的成矿系列与找矿方向
  
关键词:polymetal deposit  metallogenic series  prospecting direction  Yanshannian granites  northeastern of Hunan province
基金项目:湖南省地质院科研项目(编号: HNGSTP202306; HNGSTP202302; HNGSTP202105);中国地质调查局二级项目(编号: DD20230055; DD20221695-16);湖南省重点领域研发计划资助项目(编号: 2019SK2261);湖南省自然资源厅科技计划项目(编号: 20230102DZ)
作者单位E-mail
陈剑锋 湖南省地质调查所
湖南省地球物理地球化学调查所
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 
chenjianfeng021041@163.com 
黄建中 湖南省地质院  
文春华 湖南省地质调查所 herowch2004@163.com 
张锦煦 湖南省地质调查所  
彭薇 湖南省地质调查所  
李胜苗 湖南省地质调查所  
曹创华 湖南省地质调查所  
安江华 湖南省地质调查所  
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摘要:
A Preliminary Study of Metallogenic Series and Its Prospecting Direction Related to Yanshannian Granites in Northeastern of Hunan Province
      The northeastern Hunan Province is an important area of polymetallic (Au, Cu, Co, Pb, Zn, W) and rare-metal (Nb, Ta, Li) ore concentration in South China. The spatio-temporal distribution of polymetallic deposits and Yanshannian granites shows that the mineralization in the study area has a genetic relationship with granitoids. Based on previous studies, we hypothesize that these deposits belong to a single metallogenic series: the polymetallic (rare-metal) ore-deposit minerogenetic series related to the Yanshannian intrusion, which can be subdivided into six subseries of ore deposits. The Cu polymetallic deposit subseries (Ⅰ) associated with Early Yanshannian intrusive rocks, which is genetic realted to quzrtz porphyry orgined from Mantal-Crust interaction. The others deposit subseries (Ⅱ–Ⅵ) associated with Late Yanshannian intrusive rocks, are genetic realted to Lianyuanshan and Mufushan granitic batholith, which derived from partial melting of metasedimentary basement in an extensional tectonic setting. The Li-Nb-Ta rare-metal deposit subseries (Ⅱ) is pegmatite-type deposit formed by differentiation of two-mica monzogranite. The ore metals of the W polymetallic deposit subseries (Ⅲ) and Pb-Zn polymetallic deposit subseries (Ⅳ) were directly derived from the Mufushan granites. The ore-frrming material extracted from basement and tectonic reactivated when magma upwilling in the Lianyunshan area, supplied ore metals and migration channels for Co-Cu polymetallic deposit subseries (Ⅴ) and Au polymetallic deposit subseries (Ⅵ). Based on regional metallogenetic and “absence prospecting” theroies, this paper argue that the southern region of Changsha-Pingjiang fault has excellent prospecting for Co-Cu deposits, and the northeastern of Hunan Province showing good Au and rare-metal searchingprospects.
CHEN Jian-feng,HUANG Jian-zhong,WEN Chun-hua,ZHANG Jin-xu,PENG Wei,LI Sheng-miao,CAO Chuang-hua,AN Jiang-hua.2023.A Preliminary Study of Metallogenic Series and Its Prospecting Direction Related to Yanshannian Granites in Northeastern of Hunan Province[J].Acta Geoscientica Sinica,44(5):815-833.
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