| 彭县地区飞来峰的特征及形成演化 |
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| 引用本文： | 石绍清.彭县地区飞来峰的特征及形成演化[J].成都理工大学学报(自然科学版),1994(3). |
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| 作者姓名： | 石绍清 |
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| 作者单位： | 成都理工学院地质学系 |
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| 摘 要： | 彭县地区飞来峰根据其内部构造特征和力学成因可分为两类──推覆体和滑覆体。推覆体是挤压环境下的产物，它形成于晚三叠世末期的印支运动。滑覆体是拉张环境下重力滑动的产物，它形成于燕山──喜马拉雅期。推覆体是滑覆体的“母体”。
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| 关 键 词： | 彭县，飞来峰，推覆体，重力滑动，滑覆体，印支运动 |
CHARACTERS, FORMATION AND EVOLUTION OF THE KLIPPEN IN THE REGION OF PENGZHOU,SICHUAN |
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| Shi Shaoqing.CHARACTERS, FORMATION AND EVOLUTION OF THE KLIPPEN IN THE REGION OF PENGZHOU,SICHUAN[J].Journal of Chengdu University of Technology: Sci & Technol Ed,1994(3). |
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| Authors: | Shi Shaoqing |
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| Institution: | Shi Shaoqing |
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| Abstract: | According to the internal structural features and the mechanical origin, this paper devides the klippen in Peng County into two kinds:thruSt nappe and gliding nappe. Nappes are products formed in the compressional State by Indo-China movement in late Triassic Period. They are the original bodies of gliding nappe. Gliding nappes are products of gravity sliding formed in the Yanshan- Himalayan Period. |
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| Keywords: | Peng County klippen thrust nappe gravity sliding gliding nappe Indo-China movement |
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