Relation of thermal, velocity and gravity models of Kamchatka mantle

Deep-seated processes in the tectonosphere of geosynclines are analyzed in terms of the advection-polymorphism hypothesis. It has been shown that the said hypothesis makes it possible to explain, without resorting to numerical tailoring, major events in geological history (formation of the sedimenta...

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Bibliographic Details
Published in:IOP conference series. Earth and environmental science 2019-04, Vol.249 (1), p.12007
Main Authors: Gontovaya, L I, Gordienko, V V, Ya Gordienko, L
Format: Article
Language:English
Subjects:
Anomalies
Electrical conductivity
Electrical resistivity
Geosynclines
Gravitational fields
Heat flow
Heat transmission
Hypotheses
Polymorphism
Seismic waves
Wave velocity
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Summary:Deep-seated processes in the tectonosphere of geosynclines are analyzed in terms of the advection-polymorphism hypothesis. It has been shown that the said hypothesis makes it possible to explain, without resorting to numerical tailoring, major events in geological history (formation of the sedimentary veneer, magmatism, temperatures prevailing at large depths), as well as anomalies of the heat flow, seismic wave velocities, gravity field, and electrical conductivity.
ISSN:1755-1307
1755-1315
1755-1315
DOI:10.1088/1755-1315/249/1/012007