鄂尔多斯地块周缘地堑系形成机制及其地震活动性的实验研究
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THE EXPERIMENTAL STUDY ON THE SEISMIC ACTIVITY AND THE FORMATION MECHANISM OF GRABEN SYSTEM IN THE WESTERN PART OF NORTH CHINA
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    摘要:

    本文应用形变模拟及重力模拟对鄂尔多斯地块周缘断陷盆地带的各种特征进行了研究。认为这些断陷盆地的形成和演化主要受印度洋板块和太平洋板块共同作用而形成的拉张、剪切的力学机制控制。
    本文还应用了激光全息光弹性实验模拟地堑系的形成与地震活动的关系。同时,用定量分析法分别确定了各地堑系的应力集中区。发现鄂尔多斯地块的四个角域区应力集中较强,这与历史和现代强震震中分布基本吻合。

    Abstract:

    This paper deals with the application of deformation simulations and gravity analogy in the study of characteristic formation of graben system in the western part of North China. Experiments disclose that principal stress of the modern tectonic stress field of these graben systems is NEE-SW horizontal compression, and it is accompanied by additional vertically uplifting force from the lower crust and the upper mantle. The experimental results have confirmed that these graben systems are formed mainly due to the occurrences of tensile stress and shear stress on the axis of upheaval region of round edge of the Erdos block.
    In this paper, the seismicity here is analysed and studied, and the relation between the formation of graben system and seismicity is simulated using model experiment of laser holography photoelasticity.

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王春华,廖素琼.鄂尔多斯地块周缘地堑系形成机制及其地震活动性的实验研究[J].地震工程学报,1990,12(4):69-75. Wang Chunhua, Liao Suqiong. THE EXPERIMENTAL STUDY ON THE SEISMIC ACTIVITY AND THE FORMATION MECHANISM OF GRABEN SYSTEM IN THE WESTERN PART OF NORTH CHINA[J]. China Earthquake Engineering Journal,1990,12(4):69-75.

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  • 收稿日期:1989-12-19
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  • 在线发布日期: 2017-07-04