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Submeridional boundary zone in Asia: Seismicity, lithosphere structure, and the distribution of convective flows in the upper mantle

Research output: Contribution to journal › Article › peer-review

Seismic Imaging of the Earth Laboratory

DOI

https://doi.org/10.5800/GT-2018-9-3-0381
Final published version

N. A. Bushenkova
O. A. Kuchay
V. V. Chervov

Original language	English
Pages (from-to)	1007-1023
Number of pages	17
Journal	Geodynamics and Tectonophysics
Volume	9
Issue number	3
DOIs	https://doi.org/10.5800/GT-2018-9-3-0381
Publication status	Published - 1 Jan 2018

OECD FOS+WOS

Research areas

: continental seismicity, Central Asia, Lithosphere structure, Submeridional boundary zone, Thermal convection in the upper mantle, VELOCITY, lithosphere structure, STRONG EARTHQUAKES, ACTIVE TECTONICS, STRUCTURE BENEATH, submeridional boundary zone, CRUSTAL MOVEMENTS, FOCAL MECHANISMS, CONTINENT, thermal convection in the upper mantle, continental seismicity, TECTONIC STRESSES, RECENT GEODYNAMICS, MONGOLIA

ID: 17246692