印度洋板块边界力的不同作用方式对欧亚大陆应力场影响的实验研究
THE EXPERIMENTAL STUDY OF THE INFLUENCE OF THE DIFFERENT ACTION MODE OF INDIAN OCEAN PLATE BOUNDARY RORCE ON EURASIA STRESS FIELD
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摘要: 本文从实验角度探讨了印度洋板块边界力的不同作用方式对欧亚大陆应力场的影响。结果表明,印度洋板块带主动性的向北顶撞是造成我国西部及邻区强震三角域分布的直接原因,随边界力的作用方式由正北向北东方向偏转,大陆内部相对应力集中区条带也随之向东偏移。Abstract: From experiment angle, this paper discusses the influence of action mode of Indian ocean plate hounary force on Eurasia stress field, The results show that the northward push of Indian oeean plate zone is an immediate reason which causes strong shock triangular distribution in the west part of China and its adjacent zone, that the Indian ocean Plate zone deflects from north to northeast with the action mode of boundary force and that the zone of relative concentration of stress in the continent also deflects towards east with the action mode of bounadry force.
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