| 雪峰山陆内造山带变形特征及挤压推覆—伸展滑脱构造的物理模拟 |
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| 引用本文： | 冯向阳,孟宪刚,邵兆刚,王建平,朱大岗,赵建光.雪峰山陆内造山带变形特征及挤压推覆—伸展滑脱构造的物理模拟[J].地球学报,2001,22(5):419-424. |
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| 作者姓名： | 冯向阳 孟宪刚 邵兆刚 王建平 朱大岗 赵建光 |
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| 作者单位： | 中国地质科学院地质力学研究所，北京，100081;中国地质科学院地质力学研究所，北京，100081;中国地质科学院地质力学研究所，北京，100081;中国地质科学院地质力学研究所，北京，100081;中国地质科学院地质力学研究所，北京，100081;湖南省地质勘查局四0七队，湖南怀化418000 |
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| 基金项目： | 国家计委专项“黔阳地区金锑矿控矿条件及靶区优选”(编号95-04)，原地质矿产部地质力学开放研究实验室基金资助 |
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| 摘 要： | 本文分析了雪峰山陆内造山带的变形特征，认为雪峰山造山带是在克拉通边缘裂陷槽基础上发育起来的，历经了加里东陆缘褶皱始造山、印支－早燕山陆内褶断主造山、晚燕山－早喜马拉雅陆内盆后（重）造山等过程而最后定型的。中生代以来，岩石圈向西北的俯冲，地壳层次向西挤压产生基底滑脱、推覆增厚，进而在松弛伸展过程出现山链两侧双极性的重力滑脱。在分析变形特征的基础上，对本区的挤压推覆－伸展滑脱构造进行了物理模拟实验，实验表明，来自于SE方向的挤压作用是产生大规模的推覆－滑脱构造的动力来源。在后期的应力松弛阶段，产生伸展滑脱构造。
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| 关 键 词： | 陆内造山带 挤压推覆伸展滑脱构造 模拟实验 雪峰山 |
Deformation Features and Modeling Experiments of Nappe/Decollement Structure in Xuefeng Mountain Intracontinental Orogenic Belt |
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| FENG Xiang-yang,MENG Xian-gang,SHAO Zhao-gang,WANG Jian-ping,ZHU Da-gang and ZHAO Jian-guang.Deformation Features and Modeling Experiments of Nappe/Decollement Structure in Xuefeng Mountain Intracontinental Orogenic Belt[J].Acta Geoscientia Sinica,2001,22(5):419-424. |
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| Authors: | FENG Xiang-yang MENG Xian-gang SHAO Zhao-gang WANG Jian-ping ZHU Da-gang and ZHAO Jian-guang |
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| Institution: | Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081;Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081;Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081;Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081;Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081;No.407 Geological Party, Hunan Bureau of Geology and Mineral Resourses, Huaihua, Hunan, 418000 |
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| Abstract: | In this paper, the authors have analyzed the deformation features of Xuefeng Mountain intracontinental orogenic belt, and pointed out that Xuefeng Mountain orogenic belt was developed on the basis of the marginal rifted depressive trough of the craton, and experienced Caledonian pre-orogenic epicontinental folding, main orogenic epoch in Indosinian-Yanshanian movement, re-orogenic epoch in late Yanshanian-early Himalayan movement. From Mesozoic, the lithosphere subducted northwestward and the crust was compressed westward. The base surge and nappe were formed and thickened in middle-upper crust. The twin-polarity gravity surge was formed on each side of the orogenic belt during laxity and extension. The model experiment of nappe/decollement structure was done, and the result indicates that the pressure from southeast was the major stress that formed the nappe/decollement structures. The extension structures was formed at the stage of relaxation. |
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| Keywords: | intracontinental orogenic belt nappe/decollement structure modeling experiment Xuefeng Mountain |
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