| 晋-获断裂带分段模式研究 |
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| 引用本文： | 曹代勇,关英斌.晋-获断裂带分段模式研究[J].大地构造与成矿学,1997,21(4):323-329. |
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| 作者姓名： | 曹代勇 关英斌 |
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| 作者单位： | [1]中国矿业大学北京研究生部 [2]河北建筑科技学院 |
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| 摘 要： | 晋－获断裂带位于太行块隆与沁水块坳之间，经历了中生代道冲推覆和新生代反转伸展的构造演化进程。受基底软弱带控制，断裂带变形强度由北向南递减；由于后期隆升、剥蚀和改造的差异，呈现明显的构造分段特征。
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| 关 键 词： | 晋－获断裂带 逆冲推覆 构造反转 |
STRUCTURAL SEGMENTATION MODEL OF JINHUO FAULT ZONE |
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| Abstract: | Jinhuo fault zone lies between Taihang block uplift and Qinshui block depression,developing from a stage of thrusting in Mesozoic to a stage of tectonic inversion in Cenozoic.Controlled by the basement weak zone, deformation intensity of the zone decreased from north tosouth. Jinhuo fault zone was segmented along its strike resulting from differential uplift andreformation in later stage. |
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| Keywords: | Jinhuo fault zone thrust and nappe tectonic inversion |
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