Earthquakes generated by fluid overpressure: Insights from cryptoexplosive breccias

IF 1.7 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Jianguo Du , Fengxia Sun , Yueju Cui , Chao Xie , Fan Yang , Li Jiang
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引用次数: 3

Abstract

The genetic mechanism of earthquakes remains puzzling even though some hypotheses for earthquake generation have been proposed. A new genetic model of earthquake was established by studying the dynamical relationship between earthquake generation and cryptoexplosion. More and more cryptoexplosive breccias that were naturally produced by explosion or detonation below the surface have been found throughout the world. The endogenic cryptoexplosive breccias (CEBs) have been found at hundreds of sites in China, most of which were dated in the Yanshanian period, some in Preyanshanian, and dozen in the Himalayan period. The breccias are characterized by the angular fragments produced by hydrothermal and magmatic explosions, the network and jigsaw textures, and the matrices that originated from magma or geothermal fluids. The high energy fluids derived from the lower mantle accumulated at some places during upward migration, at which the fluid explosions occurred when the fluid pressure exceeded the confined pressure of the host rocks. As a result, innumerable paleoearthquakes were produced by the prevailing cryptoexplosions in the geological history. Such geological processes never end, as geothermal and volcanic activities do. Therefore, cryptoexplosion can be ascribed as the most primary mechanism of earthquake generation.

Abstract Image

流体超压引起的地震:来自隐爆角砾岩的见解
尽管人们提出了一些关于地震发生的假说,但地震的发生机制仍然令人困惑。通过研究地震发生与隐爆的动力学关系,建立了一种新的地震成因模型。越来越多的隐爆角砾岩在世界范围内被发现,这些隐爆角砾岩是由地表以下的自然爆炸或爆炸产生的。中国已在数百处遗址中发现了内生隐爆角砾岩(ceb),其中大部分为燕山期,部分为前燕山期,另有十几处为喜马拉雅期。角砾岩具有热液和岩浆喷发形成的角状碎块、网状和锯齿状结构、岩浆或地热流体形成的基质等特征。来自下地幔的高能流体在向上运移过程中在一些地方聚集,当流体压力超过寄主岩石的承压压力时发生流体爆炸。因此,地质历史上盛行的隐爆活动产生了无数次古地震。像地热和火山活动一样,这样的地质过程永远不会结束。因此隐爆是地震发生的最主要机制。
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来源期刊
Journal of Asian Earth Sciences: X
Journal of Asian Earth Sciences: X Earth and Planetary Sciences-Earth-Surface Processes
CiteScore
3.40
自引率
0.00%
发文量
53
审稿时长
28 weeks
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