文章摘要
曾庆栋,沈远超.胶东地区层间滑动角砾岩型金矿成矿远景[J].地质与勘探,2000,(6):36-39
胶东地区层间滑动角砾岩型金矿成矿远景
METALLOGENIC PROSPECTION OF INTERLAYER GLIDDING BRECCIA TYPE GOLD DEPOSIT IN EASTERN SHANDONG
  
DOI:
中文关键词: 层间滑动断层 角砾岩型金矿床 成矿作用机制
英文关键词: interlayer glidding fault,interlayer glidding breccia type gold deposit,metallogenic prospection,eastern Shandong
基金项目:中国科学院创新工程!(KZCX1-Y -0 3 -0 1-12 ),重大项目!(KZ95 1-A1-4 0 4-0 2 -0 2 )
曾庆栋  沈远超
中国科学院地质与地球物理研究所,北京
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中文摘要:
      胶东地区中生代盆地周边存在层间滑动断层,它控制了层间滑动角砾岩型金矿(如蓬家夼金矿)的产出,根据盆地的分布及矿化特征,划分了胶东地区四个层间滑动砾岩型金矿成矿远景区,蓬家夼成矿远景区、菜西远景区、牟平西部远景区、栖霞远景区,这些地区有望成为胶东地区甚至我国东部新的黄金工业基地。
英文摘要:
      Interlayer glidding faults develop around Mesozoic basin in eastern Shandong, these faults control the occurrence of interlayer glidding breccia type gold deposits such as Pengjiakuang gold deposit. According to distribution of Mesozoic basins and mineralization features, four metallogenic prospective areas of interlayer glidding breccia type gold deposits can be proposed in eastern Shandong: Pengjiakuang area; Laixi area; western Muping area; Qixia area, these prospective areas will be possibly become new gold industrial base of eastern Shandong in the eastern China.
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