| 试论中国内陆板块运动演化及与地震的关系 |
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| 引用本文： | 杨纪林.试论中国内陆板块运动演化及与地震的关系[J].内陆地震,2011,25(2):109-119. |
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| 作者姓名： | 杨纪林 |
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| 作者单位： | 新疆维吾尔自治区地震局,新疆,乌鲁木齐,830011 |
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| 摘 要： | 看似杂乱的中国构造形迹应是受2次大的板块运动作用形成的.第1次是西伯利亚板块运动从加里东期开始由北向南移动,大致形成山脉一盆地(海洋)相间的向南突出的巨大弧形,弧心在贝加尔一带,弧顶南部到泰国一带;西翼为北西向,从阿尔泰山到兴都库什一带;东翼为北东向,从大兴安岭到华南一带,将两翼遗留形迹与弧心联系勾画出向南突出的理想弧...
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| 关 键 词： | 内陆板块 西伯利亚板块 印度板块 构造类型 演化 |
DISCUSSION ON INTRALAND PLATE MOVING EVOLVEMENT IN CHINA AND THE RELATIONSHIP WITH EARTHQUAKE |
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| YANG Ji-lin.DISCUSSION ON INTRALAND PLATE MOVING EVOLVEMENT IN CHINA AND THE RELATIONSHIP WITH EARTHQUAKE[J].Inland Earthquake,2011,25(2):109-119. |
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| Authors: | YANG Ji-lin |
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| Institution: | YANG Ji-lin(Earthquake Administration of Xinjiang Uygur Autonomous Region,Urumqi 830011,Xinjiang,China) |
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| Abstract: | The seemingly unorderly structural configuration in China was shaped mainly by two large structural movements.The first,beginning in Caledonian period,is the Siberia plate's movement from north to south.In general,a huge southward arc,including mountain-basin and ocean,is formed.The arc's focus lies in Baikal belt.The arc's coping reaches to Thailand.The west slope is NW,from Altay to Hindu Kush belt,and the east slope is NE,from Greater Hinggan Mountains to South China.The remaining configuration of the tw... |
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| Keywords: | Intraplate Siberia plate India plate Structural configuration Evolution |
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