| 太原地区构造格局及其演化 |
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| 引用本文： | 关英斌,李海梅.太原地区构造格局及其演化[J].辽宁工程技术大学学报(自然科学版),2001,20(1):32-35. |
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| 作者姓名： | 关英斌 李海梅 |
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| 作者单位： | 河北建筑科技学院, |
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| 基金项目： | 煤炭科学基金资助项目!（95地10250）的部分科研成果。 |
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| 摘 要： | 分析了太原地区地质构造的发育规律及成因联系。研究结果表明：中生代时期，太原东山、西山矿区连为一体，共同构成了沁水向斜的西北偶；太原盆地形成使太原东、西山分离，清交等断层下盘（上升盘）的掀斜作用，使西山地区形成了向斜构造，鄂尔多斯块体的逆时针旋转，使太原东、西山地区地质构造展布方位产生了差异。
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| 关 键 词： | 构造格局 构造应力场 成因机制 太原地区 山西 |
| 文章编号： | 1008-0562(2001)01-0032-04 |
| 修稿时间： | 2000年7月13日 |
The Structural Framework and Evolution of Taiyuan Area |
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| GUAN Ying-bin,LI Hat-met.The Structural Framework and Evolution of Taiyuan Area[J].Journal of Liaoning Technical University (Natural Science Edition),2001,20(1):32-35. |
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| Authors: | GUAN Ying-bin LI Hat-met |
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| Abstract: | This paper analyzes the distribution and formation of Taiyuan area, Shanxi province. The research work shows that Dongshan and Xishan district were once a whole in Mesozoic located in the northwest part of Qinshui coal basin. The two districts were separated by the development of Taiyuan fault basin in Cenozoic. Tilfing of foot wall (up throw block) of Qingjiao fault resulted in Xishan syncline. The difference of structures extends in Dongshan and Xishan districts were resulted from the anticlockwise rotations of or Dos basin. |
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| Keywords: | structural framework stress field formation mechanism Taiyuan area |
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