地震群的流体力学

S. Bychkov
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引用次数: 0

摘要

本文所述材料的基础是液体沿管道运动时产生液压冲击的特性。地壳中的沟渠、断层和裂缝可归因于地下“管道”,岩浆可归因于液体。因此,当岩浆在地壳和地幔中运动时,就会发生液压冲击。在这个过程中产生的冲击波形成能量脉冲,伴随着温度、压力、原子的加速和减速、物质的相变和一群地震的瞬间变化。在里德先生的弹性反冲理论框架内,不可能回答地震群形成的问题,现代地球物理学犹豫不决地将此归咎于岩浆,据说它改变了地壳的温度背景,从而导致岩石的体积膨胀和震动。我们认为这种解释是正确的,但不够充分。我们认为,地震群的形成机制是岩浆在断层和岩石裂隙中运动时水力冲击的能量。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Hydrodynamics of an Earthquake Swarm
The foundation of the material described in the article is the property of a liquid during movement along the pipeline to create a hydraulic shock. Channels, faults, and cracks in the earth's crust can be attributed to underground “pipelines”, and magma to liquid. Consequently, when magma moves in the earth's crust and mantle, hydraulic shocks occur. The shock waves that arise during this process form energy pulses, which are accompanied by instantaneous changes in temperature, pressure, acceleration, and deceleration of atoms, phase transitions of matter and a swarm of earthquakes. Being within the framework of Mr. Reid's theory - Elastic recoil, it is impossible to answer the question of the formation of an earthquake swarm, and modern geophysics indecisively blames magma for this, which supposedly changes the temperature background of the earth's crust, thereby causing volumetric expansion of rocks and tremors. We find this explanation correct, but insufficient. In our opinion, the mechanism of the formation of an earthquake swarm is the energy of hydraulic shocks of magma during its movement in faults and fissures of rocks.
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