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Depth structure of the area of Klyuchevskaya group of volcanoes location according to the frequency-resonance processing of satellite images
- Publisher: European Association of Geoscientists & Engineers
- Source: Conference Proceedings, 18th International Conference on Geoinformatics - Theoretical and Applied Aspects, May 2019, Volume 2019, p.1 - 5
Abstract
The results of experimental studies carried out using the technology of frequency-resonance processing and interpretation of Earth remote sensing data (satellite images) and photo images with the aim of studying the internal structure of volcanos are analyzed. The experiments were carried out at sites of the location of the famous Klyuchevskaya group of volcanic complexes. The results of the deep frequency-resonance sounding of the cross-section in the surveyed area show that the roots of the volcanoes existing here (channels of deep fluids and mineral matter migration) are located in the molten (liquid) rock layer, which is detected and fixed on the globe almost everywhere in the depth interval of 194–225 km, as well as at depths of 470 km and 723 km. Within the three surveyed areas, kimberlite pipes with diamond inclusions, as well as a channel of the mineral matter migration, were found. The materials of the research carried out in the area of the Klyuchevskaya group of volcanoes in Kamchatka can be considered as confirmation of the assumptions that volcanic structures can be a source of hydrogen. Operatively conducted experimental studies have shown that the frequency-resonance method of Earth remote sensing data processing and interpreting can be used to study the deep structure of the Earth's tectonic structures and to search for combustible and ore minerals.