| 赣北大湖塘钨多金属矿田区域地质特征研究* |
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| 引用本文： | 张志辉,耿林,贾文彬,巩小栋,杜泽忠,张明超.赣北大湖塘钨多金属矿田区域地质特征研究*[J].中国矿业,2014,23(14). |
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| 作者姓名： | 张志辉 耿林 贾文彬 巩小栋 杜泽忠 张明超 |
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| 作者单位： | 中国地质调查局发展研究中心,中国地质调查局发展研究中心,中国地质大学北京,中国地质大学北京,中国地质调查局发展研究中心,中国地质大学北京 |
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| 摘 要： | 赣北大湖塘钨矿田大地构造位置位于扬子陆块区-下扬子陆块-江南古岛弧的中北部,其北临幕阜山(鄂东)被动边缘盆地,南接宣春断陷盆地。区域出露有中元古代、新元古代、古生代和中生代地层,其中以中元古代地层最发育,新元古代、古生代、中生代地层零星出露。区内经历了多次构造活动,其中晋宁运动、印支运动和燕山运动最为醒目,表现为强烈的褶皱和断裂广泛发育。
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| 关 键 词： | 赣北 大湖塘 钨矿 地质特征 |
| 收稿时间： | 2014/11/20 0:00:00 |
| 修稿时间： | 2014/11/20 0:00:00 |
Tungsten-polymetallic ore field, regional geological characteristics study , Datanghu tungsten polymetallic deposit in Gan bei |
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| ZHANG Zhi-hui,GENG Lin,JIA Wen-bin,GONG Xiao-dong,DU Ze-zhong and ZHNAG Ming-chao.Tungsten-polymetallic ore field, regional geological characteristics study , Datanghu tungsten polymetallic deposit in Gan bei[J].China Mining Magazine,2014,23(14). |
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| Authors: | ZHANG Zhi-hui GENG Lin JIA Wen-bin GONG Xiao-dong DU Ze-zhong and ZHNAG Ming-chao |
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| Affiliation: | Development and Research centre,China Geological Survey,Beijing,Development and Research centre,China Geological Survey,Beijing,China University of Geosciences,Beijing,China University of Geosciences,Beijing,Development and Research centre,China Geological Survey,Beijing,China University of Geosciences,Beijing |
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| Abstract: | Dahutang tungsten ore field in north of Jiangxi province is located in the Yangtze continental block-of-lower Yangtze Jiangnan Proterozoic in the Northern, mufu mountain in the North (Hubei Province), passive margin basins, Xuan Chun rift basin in the South. Regional outcropping Proterozoic, neoproterozoic and Paleozoic and Mesozoic strata, with middle Proterozoic strata are most developed, neoproterozoic, Paleozoic, Mesozoic strata scattered outcrops. Has experienced a number of tectonic activity in the district, jinning movement, Indo-China yanshanian movement in sport and the most eye-catching, characterized by widely developed strong folds and faults. |
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| Keywords: | Ganbei Dahutang Tungsten Geological characteristics |
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