ORIGIN OF THE MOUNTAINS IN THE SOUTH OF THE RUSSIAN FAR EAST (Paper 1. Orogenic belts)
https://doi.org/10.15356/0435-4281-2014-3-3-16
Abstract
There are several alternative tectonic models of the Far East mountains origin: geosynclinal folding, lineamentblock neotectonic uprise, tectono-magmatic activation, tectonic and morphogenetic processes connected with local magmatic centers, horst-accretional and graben-rift tectonics, terrain or plume tectonics. By authors’ opinion the main features of morphostructure pattern of orogenes (deep “roots”, sub-parallel location, translational distribution of large watershed junctions, etc.) may be reasonably explained only on the basis of plume tectonics and of morphogenetic processes connected with magmatic centers. The structural frame of the orogenic belts territory is formed by linear systems of arch-block and tectonic-magmatic uplifts. Their origin and development are conditioned by periodic activation and general evolution of the Circum-Pacific deep faults of the East-Asian overplume mega-arch and its satellite magmatic centers during the sustainable Late Mesozoic-Early Cenozoic eastward migration of the front of acid magmatism and westward migration of the front of the mafic one.
About the Author
A. A. Gavrilov
Il'ichev Pacific Oceanological Institute FEB RAS, Vladivostok
Russian Federation
Russian Federation
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Review
For citations:
Gavrilov A.A. ORIGIN OF THE MOUNTAINS IN THE SOUTH OF THE RUSSIAN FAR EAST (Paper 1. Orogenic belts). Geomorfologiya. 2014;(3):3-16. (In Russ.) https://doi.org/10.15356/0435-4281-2014-3-3-16
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