张裕明. 可可托海-二台断层第四纪活动的地表特征和粘滑运动的地质证据[J]. 华北地震科学, 1986, 4(4): 45-52.
引用本文: 张裕明. 可可托海-二台断层第四纪活动的地表特征和粘滑运动的地质证据[J]. 华北地震科学, 1986, 4(4): 45-52.
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Zhang Yuming. SURFACE CHARACTERISTICS OF QUATERNARY ACTIVITY AND GEOLOGICAL EVIDENCES OF STICK SLIP MOVEMENT OF KEKETUO OCEAN-ERTAI FAULT[J]. North China Earthquake Sciences, 1986, 4(4): 45-52.
Citation: Zhang Yuming. SURFACE CHARACTERISTICS OF QUATERNARY ACTIVITY AND GEOLOGICAL EVIDENCES OF STICK SLIP MOVEMENT OF KEKETUO OCEAN-ERTAI FAULT[J]. North China Earthquake Sciences, 1986, 4(4): 45-52.
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可可托海-二台断层第四纪活动的地表特征和粘滑运动的地质证据

SURFACE CHARACTERISTICS OF QUATERNARY ACTIVITY AND GEOLOGICAL EVIDENCES OF STICK SLIP MOVEMENT OF KEKETUO OCEAN-ERTAI FAULT

    摘要
  • 摘要: 本文研究了可可托海一二台断层第四纪以来沿断层发生大规模右旋走滑和倾滑运动在地表留下的各种痕迹,并对其现代运动的力学特性——粘滑机制提出了地质证据。

     

    Abstract: In this paper, a variety of marks that were left on the surface after massive rightlateral strike slip and dip slip movement along faults since Quaternaty in Keketuo Hai-Ertai futlts are studidl. At the same time, geological evidences are suggested for mechanical behavior of recent movement stick slip mechanism.

     

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