湖北省随县王家台金多金属矿地球化学特征及矿床成因初探
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摘要
王家台矿区位于湖北省随县北部黑龙潭金矿的北西侧,地处东秦岭Au-Ag-Mo-Cu-Pb-Zn-Sb金属成矿带之随枣地区金银成矿亚带,通过矿区主量元素、微量元素和稀土元素地球化学特征研究,初步归纳成矿元素的富集规律,认为其成因类型为与燕山期构造—岩浆热液作用有关的蚀变岩型、石英脉型金多金属矿。
The Wangjiatai mining area is located at the northwest side of the Heilongtan gold deposit in the northern part of Suixian,Hubei province. It is located in the gold-silver metallogenic belt of Suizhou-Zaoyang area in the Au-Ag-MoCu-Pb-Zn-Sb metallic metallogenic belt of the eastern Qinling Mountains. Through the results of geochemical studies of the major elements,trace elements and rare earth elements in the mining area,the enriching regularity of ore forming elements are summarized,it is preliminarily believed that the genetic type is the altered rock type and quartz vein type gold polymetallic ore related to the Yanshanian tectonic-magmatism.
The Wangjiatai mining area is located at the northwest side of the Heilongtan gold deposit in the northern part of Suixian,Hubei province. It is located in the gold-silver metallogenic belt of Suizhou-Zaoyang area in the Au-Ag-MoCu-Pb-Zn-Sb metallic metallogenic belt of the eastern Qinling Mountains. Through the results of geochemical studies of the major elements,trace elements and rare earth elements in the mining area,the enriching regularity of ore forming elements are summarized,it is preliminarily believed that the genetic type is the altered rock type and quartz vein type gold polymetallic ore related to the Yanshanian tectonic-magmatism.
引文
[1]谭秋明.湖北随北地区金银成矿地质条件分析[J].湖北地质,1994,8(2):51-58.
[2]钟增球,索书田,徐启东,等.桐柏—大别造山带剪切带阵列的构造岩研究[J].地质学报,1996,70(4):313-323.
[3]刘腾飞.鄂北地区韧性剪切带的地质特征及含矿性研究[J].黄金科学技术,1994,2(3):29-32.
[4]刘腾飞.鄂北黑龙潭剪切带型金矿床地质特征及成因[J].黄金地质科技,1994(4):11-17.
[5]陈超,毛新武,彭少南,等.鄂北七尖峰岩体LA-ICP-MS锆石U-Pb测年及其岩石成因、成矿意义[J].资源环境与工程,2018,32(2):167-172.
[6]胡起生,许天良,黄国平,等.湖北黑龙潭金矿矿床成因及成矿模式[J].湖北地矿,2003,17(1):9-13.
[7]李书涛.湖北随枣地区黑龙潭—封江金矿田成矿特征及控矿因素研究[J].国外前寒武纪地质,1996,76(4):43-56.
[8]彭三国,胡俊良,刘劲松,等.湖北随州黑龙潭金矿石英Rb-Sr同位素年龄及其地质意义[J].地质通报,2017,36(5):867-874.
[9]周豹,朱金,刘文文,等.湖北随县王家台金银钨多金属矿地质特征、矿床成因及找矿方向浅析[J].资源环境与工程,2018,32(3):358-361.
[10]胡中岳,胡起生,黄国平,等.湖北随州市七尖峰地区伸展构造与成矿[J].资源环境与工程,2004,18(4):9-16.
[11]彭万俊,胡起生,黄国平,等.湖北省随枣北部地区银金矿成矿条件及找矿前景[J].资源环境与工程,2004,18(增刊):48-53.
[12]冷双梁,匡华,谭超,等.随—枣七尖峰岩体周缘金矿床特征对比及成矿过程初探[J].资源环境与工程,2015,29(3):275-279.
[2]钟增球,索书田,徐启东,等.桐柏—大别造山带剪切带阵列的构造岩研究[J].地质学报,1996,70(4):313-323.
[3]刘腾飞.鄂北地区韧性剪切带的地质特征及含矿性研究[J].黄金科学技术,1994,2(3):29-32.
[4]刘腾飞.鄂北黑龙潭剪切带型金矿床地质特征及成因[J].黄金地质科技,1994(4):11-17.
[5]陈超,毛新武,彭少南,等.鄂北七尖峰岩体LA-ICP-MS锆石U-Pb测年及其岩石成因、成矿意义[J].资源环境与工程,2018,32(2):167-172.
[6]胡起生,许天良,黄国平,等.湖北黑龙潭金矿矿床成因及成矿模式[J].湖北地矿,2003,17(1):9-13.
[7]李书涛.湖北随枣地区黑龙潭—封江金矿田成矿特征及控矿因素研究[J].国外前寒武纪地质,1996,76(4):43-56.
[8]彭三国,胡俊良,刘劲松,等.湖北随州黑龙潭金矿石英Rb-Sr同位素年龄及其地质意义[J].地质通报,2017,36(5):867-874.
[9]周豹,朱金,刘文文,等.湖北随县王家台金银钨多金属矿地质特征、矿床成因及找矿方向浅析[J].资源环境与工程,2018,32(3):358-361.
[10]胡中岳,胡起生,黄国平,等.湖北随州市七尖峰地区伸展构造与成矿[J].资源环境与工程,2004,18(4):9-16.
[11]彭万俊,胡起生,黄国平,等.湖北省随枣北部地区银金矿成矿条件及找矿前景[J].资源环境与工程,2004,18(增刊):48-53.
[12]冷双梁,匡华,谭超,等.随—枣七尖峰岩体周缘金矿床特征对比及成矿过程初探[J].资源环境与工程,2015,29(3):275-279.