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Integral evolution pattern of intraplate seismicity in Chinese mainland and its periphery

机译:中国大陆及其周边地区板内地震活动的整体演化模式

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摘要

Taking the active fault network as the structural frame, the Chinese mainland and its periphery can be regarded as a system of "fault movement and seismogeny." By using the self-coupling method, preliminary study shows that the seismogenic system is a time- ordered dissipation system. The time order in the state far from equilibrium is established and maintained through mass and energy exchanges between the system and the surroundings.
机译:以活动断层网络为结构框架,中国大陆及其周边地区可以看作是一个“断层运动和地震成因”系统。通过使用自耦合方法,初步研究表明,震源系统是时间有序的耗散系统。通过系统与周围环境之间的质量和能量交换,可以建立并保持状态中远离平衡状态的时间顺序。

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