The significance of the rotation factor in continuous geodynamics

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The article deals with the problem of taking into account the rotational factor in the study of continuous geodynamics in a single natural system of different ranks movements. The significance of transit thalwegs is shown - indicators of the dominant process of matter compaction to the center Earth. The fractal structure of natural control, in which the Kamchatka peninsula develops, is given. Two opposite regimes of the Earth the development during the day during the rotation of the planet around its axis are reflected. The distribution of earthquakes is shown depending on their localization, magnitude and mode of the Earth's development during the day. This information is necessary for the development of technologies for predicting and reducing the manifestations of negative natural processes, including earthquakes.

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Transit thalweg, hydro- and lithodynamic flow, continuous geodynamics, natural control of movements, increased compaction of matter, rotation of the earth around its axis, earthquake

Короткий адрес: https://sciup.org/170194804

IDR: 170194804   |   DOI: 10.24412/2500-1000-2022-6-1-90-99

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