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VELOCITY OF THE SUBDUCTION OF THE RUSSIAN PLATFORM UNDER THE SIBERIAN ONE IN THE PALEOZOIC BY THE DISTRIBUTION OF MANTLE HYDRO-CARBON UPWELLING ZONES IN WESTERN SIBERIA
1 Schmidt Institute of Physics of the Earth, RAS, Moscow, Russia
2 Pushkov Institute of Terrestrial Magnetism, Ionosphere and Radio Wave Propagation, RAS, Moscow, Russia
2 Pushkov Institute of Terrestrial Magnetism, Ionosphere and Radio Wave Propagation, RAS, Moscow, Russia
Journal: Geophysical research
Tome: 16
Number: 4
Year: 2015
Pages: 36-40
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Gavrilov S., Kharitonov A. VELOCITY OF THE SUBDUCTION OF THE RUSSIAN PLATFORM UNDER THE SIBERIAN ONE IN THE PALEOZOIC BY THE DISTRIBUTION OF MANTLE HYDRO-CARBON UPWELLING ZONES IN WESTERN SIBERIA // . 2015. Т. 16. № 4. С. 36-40.
@article{GavrilovVELOCITY2015,
author = "Gavrilov, S. and Kharitonov, A.",
title = "VELOCITY OF THE SUBDUCTION OF THE RUSSIAN PLATFORM UNDER THE SIBERIAN ONE IN THE PALEOZOIC BY THE DISTRIBUTION OF MANTLE HYDRO-CARBON UPWELLING ZONES IN WESTERN SIBERIA",
journal = "Geophysical research",
year = 2015,
volume = "16",
number = "4",
pages = "36-40",
doi = "",
language = "English"
}
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Keywords: non-organic hydrocarbons transport, mantle wedge convection, subduction angle and velocity
Аnnotation: VELOCITY OF THE SUBDUCTION OF THE RUSSIAN PLATFORM UNDER THE SIBERIAN ONE IN THE PALEOZOIC BY THE DISTRIBUTION OF MANTLE HYDRO-CARBON UPWELLING ZONES IN WESTERN SIBERIA
