The study of the thermo-baric parameters of the mantle environment within the territory of the Pacific mantle plume by satellite and ground geophysical data
The purpose of this article is to show the results of the study of thermo-baric parameters and deep structure of the Earth's mantle in order to identify possible subvertical channels of migration of deep hydrocarbons to its surface. Various satellite and ground geophysical data are analysed to meet this challenge. Using satellite measurements of the geomagnetic field, vertical cross-sections of various physical parameters of the depth structure of the mantle were constructed for the territory of the Pacific mantle plume, based on solving inverse problems of potential theory and classical equations of electromagnetic dynamics. One of the main subvertical channels for the transfer of deep hydrocarbons to the Earth's surface has been shown to be mantle plumes.