| 中国构造应力场特征及其与板块运动的关系 |
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| 引用本文： | 邓起东
,张裕明
,许桂林
,范福田.中国构造应力场特征及其与板块运动的关系[J].地震地质,1979,1(1):11. |
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| 作者姓名： | 邓起东 张裕明 许桂林 范福田 |
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| 摘 要： | 本文根据地质构造、地震和地壳形变等资料,研究了中国晚第三纪以来构造应力场的主要特征。认为,中国区域构造应力场有明显的分区特点:构造应力场以水平分量为主,但某些地区由于深部物质运动可以同时存在垂直附加力的作用;同时认为,中国构造应力场是受印度板块和太平洋板块的联合作用控制的
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| 关 键 词： | 现代构造应力场 断块区 北北东向 板块运动 主压应力轴 新构造 逆断层 弧形构造带 青藏 北西向 |
ON THE TECTONIC STRESS FIELD IN CHINA AND ITS RELATION TO PLATE MOVEMENT |
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| Abstract: | Basing upon the data of geological and seismological observations and crustal deformation this paper deals mainly with the characteristics of the tectonic stress field in China since Late Tertiary. Such a tectonic stress field is characterized first of all by obvious zonations. And it is especially distinct in three broad regions, namely West China, North China-Northeast China and South China-Taiwan. The tectonic stress field in these regions seems to be stable.The mechanical behavior of tectoni |
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