| 中国大陆余震活动深度分布及其流变学机制 |
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| 引用本文： | 傅征祥.中国大陆余震活动深度分布及其流变学机制[J].中国地震,1996,12(2):147-154. |
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| 作者姓名： | 傅征祥 |
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| 作者单位： | 国家地震局分析预报中心 100036 |
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| 摘 要： | 本文研究了中国大陆１９６６年以来发生的５次大地震（Ｍｓ≥７．０）的余震活动深度与地热流的关系。研究表明，地热流较高的震源区，余震活动深度分布较浅，并且得出余震深度分布受地壳内部岩石脆性－韧性转变深度的流变学特征控制的推论。
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| 关 键 词： | 余震深度 地热流 流变学 地震活动性 |
Distribution of Aftershock Deepths in China Mainland and Its Rheological Mechanism |
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| Fu Zhengxiang.Distribution of Aftershock Deepths in China Mainland and Its Rheological Mechanism[J].Earthquake Research in China,1996,12(2):147-154. |
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| Authors: | Fu Zhengxiang |
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| Abstract: | The relationship between aftershock depths and surface heat flow in the source areas of five great earthquakes (Ms>7. 0) in China mainland has been studied in the paper, it shows that the higher the surface heat flow, the more shallow the aftershock depths , and distribution of aftershock depths are under the control of the rheological mecha -nism of the rock brittle-ductile transition in the crust. |
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| Keywords: | Aftershock depths Surface heat flow Rheology |
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