Terranes of the Verkhoyansk fold-and-thrust belt, East Yakutia
https://doi.org/10.31242/2618-9712-2019-24-4-5
Abstract
The origin and tectonic pattern of terranes of the Verkhoyansk fold-and-thrust belt are still not clearly understood. The studies of the terranes are mostly based on a variety of assumptions which, in turn, give rise to new ones. This causes a number of questions, some of which are discussed in the present paper. One of the solutions to this problem is that the Verkhoyansk-Kolyma Mesozoides system (VKMS) was formed in the Middle Jurassic–Early Cretaceous as a result of a collision of the Siberian continent with the Earth’s crust blocks or minor oceans, marginal seas, back-arc basins, microcontinents, and island arcs, which were located within the pericratonal convergent zone or in the rear part of the convergent boundary framing the shore of the North Asian continent. A characteristic feature of the VKMS terranes is that they are collisional terranes forming orogenic systems with an isometric mosaic pattern, which differ from linear orogenic systems composed of accretionary terranes.
Keywords
terrane,
tectonic accretion,
convergent boundary,
collision,
pericratonal convergent zone,
Verkhoyansk-Kolyma Mesozoides system
Supporting agencies: The work was done as part of Research Program of DPMGI, SB RAS (project no. 0381-2019-0001, and was partly supported by grant no. 19-05-00945 from RFBR
About the Author
Felix Filaretovich Tretyakov
Diamond and Precious Metal Geology Institute SB RAS
Russian Federation
Russian Federation
Tretyakov Felix Filaretovich, candidate of geological and mineralogical sciences, senior researcher, Diamond and Precious Metal Geology Institute SB RAS, 39 Lenina pr., Yakutsk, 677980, Russia, https://orcid.org/0000-0003-3911-2491, tretyakov_ff@mail.ru.
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For citations:
Tretyakov F.F. Terranes of the Verkhoyansk fold-and-thrust belt, East Yakutia. Arctic and Subarctic Natural Resources. 2019;24(4):67-78. (In Russ.) https://doi.org/10.31242/2618-9712-2019-24-4-5
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