The earth's absolute gravitation potential function in the prospect 'gravitational potential metering' of geological objects and earthquake centers
Aleksandr Fridrikson, Marina Kasatochkina

TL;DR
This paper introduces a method for detecting Earth's maximum gravitation potential and its relation to geological structures and earthquakes, using the Vs-gravity method to improve understanding of Earth's interior and seismic activity.
Contribution
The paper presents a novel approach to measure Earth's absolute gravitation potential and locate maximum gravitation points, linking them to seismic layers and earthquake prediction.
Findings
Earth's maximum gravitation coincides with the D'' seismic layer.
The Vs-gravity method effectively detects low-power or distant geological objects.
The method shows promise for earthquake prediction and geological exploration.
Abstract
The direct problem of the detection of the Earth's absolute gravitation potential maximum value (MGP) was solved. The inverse problem finding of the Earth maximum gravitation (where there is a maximum of gravitation field intensity and a potential function has a 'bending point') with the help of MGP was solved as well. The obtained results show that the revealed Earth maximum gravitation coincides quite strictly with the cseismic D" layer on the border of the inner and outer (liquid) core. The validity of the method of an absolute gravitation potential detection by the equal- potential velocity was proved as 'gravitation potential measurement' or 'Vs-gravity method'. The prospects of this method for detecting of low-power or distant geological objects with abnormal density and the possible earthquakes with low density was shown.
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Taxonomy
TopicsEarthquake Detection and Analysis · Statistical and numerical algorithms · Mining and Gasification Technologies
