ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
汉南金水-青泥坑镁铁层状杂岩体岩石层序与铂矿化
  
关键词:mafic layered complex  rocksequence  Pt-deposits  Jinshui-Qingnikeng Hannan
基金项目:
作者单位
杨星 西安地质矿产研究所 
潘小平 西安地质矿产研究所 
姚文光 西安地质矿产研究所 
杨建国 西安地质矿产研究所 
杨合群 西安地质矿产研究所 
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摘要:
Mafic Layered Comples Body and Its Platinum-Bearing Nature in Jinshui-Qingnikeng Hannan
      Jinshuui-Qingnikeng mafic layered complex body is located north rim of Yangtze plate, east-north position of Hannan terrain.It intrudes into Xixiang Group,out-cropping, more than 500km2 and is mainly composed of gabbroites, partly ultramafic py-roxenite and peridotite. According to layered rock-sequence and types, the body is divided into two zones; the upper gabbroites and the lower zone composed of pyroxenite, peridotite and coarse altered gabbroite. It is studied that evolution of petrochemisry, mineral chemistry and trace element geochemistry is consistent with that of layered rock sequence. The position of developing rhythemtic units shows there had been many time emplacement activity of magma forming complex body. Besides, this paper has shown that the total value of REE and (La/Yb)N increase with rise of layered rock sequence yet, those coincidence with general low of REE fractionation tendency. In this paper, a systematic explantion for PGE distribution characteristics of various rocks in the complex body has been made, and the occurrence places of mineralization of Pt and Cu-Ni has preliminarily been determined and minerogenesis of PGE has also been dis-cussed. After analysing geological tectonic environment in which the complex body forms, it is discussed character of parental magma, and estimated partly melting degree.
Yang Xing,Pan Xiaoping,Yao Wenguang,Yang Jianguo,Yang Hequn.1996.Mafic Layered Comples Body and Its Platinum-Bearing Nature in Jinshui-Qingnikeng Hannan[J].Acta Geoscientica Sinica,17(z1):43-49.
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