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郯庐断裂与金矿成矿
引用本文:沈远超,曾庆栋,刘铁兵,李光明,申萍,孙秀英.郯庐断裂与金矿成矿[J].世界地质,2003,22(1):41-44.
作者姓名:沈远超  曾庆栋  刘铁兵  李光明  申萍  孙秀英
作者单位:中国科学院地质与地球物理研究所,北京,100029
基金项目:国家十五科技攻关项目 ( 2 0 0 1BA60 9A 0 7 0 8),中国科学院创新工程项目 (KZCX3 SW 13 7)资助
摘    要:郯庐断裂带是我国东部规模巨大的北东向断裂构造系,长约2500km。南起庐江至郯城,经渤海向北,分成伊兰-舒兰断裂和敦化-密山断裂。不同区域、不同时代具有不同特征。郯庐断裂控制了许多大型、中型和小型金矿分布,是中国最大的金矿成矿带。

关 键 词:郯庐断裂  金矿  中国东部
文章编号:1004-5589(2003)01-0041-04

The Tanlu Fault Zone and Gold Ore Metallogenesis
Shen Yuan-chao,Zeng Qing-dong,Liu Tie-bing Li Guang-ming,Shen Ping,Sun Xiu-ying Institute of Geology,Chinese Academy of Sciences,Beijing ,China.The Tanlu Fault Zone and Gold Ore Metallogenesis[J].World Geology,2003,22(1):41-44.
Authors:Shen Yuan-chao  Zeng Qing-dong  Liu Tie-bing Li Guang-ming  Shen Ping  Sun Xiu-ying Institute of Geology  Chinese Academy of Sciences  Beijing  China
Institution:Shen Yuan-chao,Zeng Qing-dong,Liu Tie-bing Li Guang-ming,Shen Ping,Sun Xiu-ying Institute of Geology,Chinese Academy of Sciences,Beijing 100029,China
Abstract:The Tanlu Fault Zone (TFZ) is a large NE-trending deep fracture system in easten China and about 2 500 km long. It extends from the south of Lujiang to Tancheng,and passes through the Bohai Sea and continues to the north,where it branches into the Yilan-Shulan Fault and Dunhua-Mishan Fault. The TFZ is a long lasting huge deep-rooted lithospherical fault system with waried characteristics in different parts and at different periods in its evolution. The TFZ is the largest gold metallogenic zone,and controls of many superlarge,large,middle and small sized gold ore deposits in their forming and distributions.
Keywords:Tanlu fault zone  gold deposit  eastern China
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