| 柞山泥盆纪沉积盆地成矿动力学分析 |
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| 引用本文： | 方维萱.柞山泥盆纪沉积盆地成矿动力学分析[J].矿产与地质,1999,13(3):141-147. |
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| 作者姓名： | 方维萱 |
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| 作者单位： | 西北大学地质系,西安,710069 |
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| 摘 要： | 造成热水成矿流体大规模迁移的机理有地壳的伸展、挤压、旋转伸展与旋转挤压。盆地中同生断裂是热水成矿流体迁移和传输的通道，沉积盆地是其沉淀和定位的场所，盆地的反转是矿床保存的条件，研究柞水泥盆纪沉积盆地的成矿动力学特征。
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| 关 键 词： | 沉积盆地 大陆动力学 流体成矿动力学 盆地的改造 柞山盆地 |
| 修稿时间： | 1998年12月28日 |
RESEARCH ON GEODYNAMICS OF ZASHAN SEDIMENTARY BASIN |
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| Fang Weixuan.RESEARCH ON GEODYNAMICS OF ZASHAN SEDIMENTARY BASIN[J].Mineral Resources and Geology,1999,13(3):141-147. |
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| Authors: | Fang Weixuan |
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| Abstract: | Largescale migrating
mechanisms of oreforming hydrothermal fluids,include extension,compression,rotational
extension and rotational compression at the earth crust.Synsedimentary faults in the
sedimentary basin are passages of migrating and transfering for oreforming hydrothermal fluid,
while the sedimentary basin is the place for precipitation and location of oreforming
hydrothermal fluids.Deposits are well covered by reversing of the sedimentary basin.The
characterization of geodynamics of the sedimentary Basin in Zashan,is also studied in the
paper. |
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| Keywords: | Sedimentary basin Continent dynamics Dynamics of oreforming fluid Modification of basin Zashan basin |
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