| 滥木厂铊矿床控矿断裂构造形成的动力学机制 |
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| 引用本文： | 任大银,陈代演.滥木厂铊矿床控矿断裂构造形成的动力学机制[J].贵州教育学院学报,2006,17(4):50-54. |
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| 作者姓名： | 任大银 陈代演 |
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| 作者单位： | 贵州教育学院地理系 贵州贵阳550003(任大银)，贵州大学资源与环境学院 贵州贵阳550003(陈代演) |
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| 摘 要： | 滥木厂铊矿床产于NE向滥木厂鼻状背斜核部和近核部,并严格受控于与背斜关系密切的NE向断裂组。实际地质资料和模拟实验研究都表明,该矿床控矿断裂为同成矿断裂。对该矿床同成断裂形成的动力学机制研究表明,其受多种因素控制。
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| 关 键 词： | 控矿断裂 铊矿床 滥木厂 动力学机制 |
| 文章编号： | 1002-6983（2006）04-0050-05 |
| 收稿时间： | 2006-05-15 |
| 修稿时间： | 2006年5月15日 |
The forming dynamical mechanisms of ore-controlling faults on Lanmuchang Thalliun deport |
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| REN Da-yin,CHEN Dai-yan.The forming dynamical mechanisms of ore-controlling faults on Lanmuchang Thalliun deport[J].Journal of Guizhou Educational College(Social Science Edition),2006,17(4):50-54. |
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| Authors: | REN Da-yin CHEN Dai-yan |
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| Institution: | 1. Department of Geology, Guizhou Education lustitute, Guiyang, Guizhou 550003, China; 2. Resource and Environment College,Guizhou University,Guiyang, Guizhou 550003, China |
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| Abstract: | The Lamuchang Thallium deposit occurs in the core and near the core of the NE Lanmuchang anticline,and is controlled by NE-SW faults,which have relationship with the Lanmuchang anticline.Geological data and experimental data demonstrate that:ore-controlling faults are simultaneity-metallogenesis faults in this deposit.In this paper,writer mainly stadies the forming dynamical mechanisms of simultaneity-metallogenesis faults in this deposit. |
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| Keywords: | ore-controlling faults Thallium deposit Lanmuchang Guizhou province |
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