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The Earth's decelerated rotation and regularities in orientation of its surface lineaments and faults

机译:地球减速的自转和表面线和断层定向的规律性

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摘要

The Earth's crust faults and lineaments group in clusters with predominant N-S and E-W (System Ⅰ) and NW-SE and NE-SW (System Ⅱ) directions. The earthquake epicenters of the Benioff seismofocal zones follow the same regularities. In other words, seismofocal zones (epicenters of earthquakes) constitute a part of the regular network of the Earth's crust and lithosphere faults and lineaments. Mathematical modeling of stress distribution in the lithosphere due to a change of the Earth's ellipsoid compression showed that the principal stresses σ_1 and σ_2 are oriented in N-S and E-W directions, while corresponding shear stresses t are oriented in NE-SW and NW-SE directions. It is shown that the secular deceleration of the Earth's rotation can be a reasonable mechanism for the change of Earth's ellipsoid compression and, consequently, for the origin of the regular system of faults and lineaments described above.
机译:地壳断层和质系群以N-S和E-W(系统Ⅰ)为主,NW-SE和NE-SW(系统Ⅱ)为主。贝尼奥夫地震带地区的地震震中遵循相同的规律。换句话说,地震海床区(地震的震中)构成了地壳,岩石圈断层和构造的常规网络的一部分。地球椭球压缩变化引起的岩石圈应力分布的数学模型表明,主应力σ_1和σ_2定向在N-S和E-W方向,而相应的切应力t定向在NE-SW和NW-SE方向。结果表明,地球自转的长期减速可能是改变地球椭球压缩力的合理机制,因此,对于上述断层和构造常规系统的起源也可能是合理的。

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