| 宁夏地质梗要 |
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| 引用本文： | 霍福臣.宁夏地质梗要[J].甘肃地质学报,1993(Z1):101-133. |
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| 作者姓名： | 霍福臣 |
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| 作者单位： | 甘肃省地质矿产局 兰州 |
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| 摘 要： | 宁夏位于中朝准地台和昆仑秦岭地槽褶皱区两大地质构造单元的衔接部位。区内各时代地层均有出露;岩浆岩不发育;构造运动活跃。该区地质构造的演化大致经历了4个阶段。
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| 关 键 词： | 宁夏 地层 构造运动 岩桨岩 演化 |
THE GEOLOGICAL OUTLINE IN NINGXIA HUI AUTONOMOUS REGION |
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| Huo Fuchen.THE GEOLOGICAL OUTLINE IN NINGXIA HUI AUTONOMOUS REGION[J].Acta Geologica Gansu,1993(Z1):101-133. |
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| Authors: | Huo Fuchen |
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| Institution: | Huo Fuchen (Bureau of Geology and Mineral Resources of Gansu Province, Lanzhou 730000) |
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| Abstract: | Ningxia is situated on the border of two geological structure units which is Sino -Korean paraplatform and Qinling geosyncline folded belt. The different epoch strata are present, but magmatite is not well development and tectonic movement is active frequently in the area. The tectonic evolution had undergone about four stages in this regipn. |
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| Keywords: | Ningxia Stratum Tectonic movement Magmatit Evolution |
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