gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2017-8-3-0256gtcrust-397Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSORIGIN OF MELTING ANOMALIES IN THE JAPAN-BAIKAL CORRIDOR OF ASIA AT THE LATEST GEODYNAMIC STAGE: EVOLUTION FROM THE MANTLE TRANSITION LAYER AND GENERATION BY LITHOSPHERIC TRANSTENSIONORIGIN OF MELTING ANOMALIES IN THE JAPAN-BAIKAL CORRIDOR OF ASIA AT THE LATEST GEODYNAMIC STAGE: EVOLUTION FROM THE MANTLE TRANSITION LAYER AND GENERATION BY LITHOSPHERIC TRANSTENSIONChuvashovaI. S.ChuvashovaI. S.

Irkutsk

Irkutsk

RasskazovS. V.RasskazovS. V.

Irkutsk

Irkutsk

SunYi-minSunYi-min

Wudalianchi, Heilongjiang 164155

Wudalianchi, Heilongjiang 164155

YangChenYangChen

Wudalianchi, Heilongjiang 164155

Wudalianchi, Heilongjiang 164155

Institute of the Earth's Crust, Siberian Branch of RAS; Irkutsk State UniversityРоссияInstitute of the Earth's Crust, Siberian Branch of RAS; Irkutsk State UniversityRussian FederationInstitute of Volcanoes and Mineral Springs, Heilongjiang Academy of ScienceКитайInstitute of Volcanoes and Mineral Springs, Heilongjiang Academy of ScienceChina20171010201783435440Copyright © Chuvashova I.S., Rasskazov S.V., Sun Y., Yang C., 20172017Chuvashova I.S., Rasskazov S.V., Sun Y., Yang C.Chuvashova I.S., Rasskazov S.V., Sun Y., Yang C.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.gt-crust.ru/jour/article/view/397

At the latest geodynamic stage that is characterized by forces and processes of the last 90 Ma the lithosphere of Asia has been reactivated due to four main force factors: 1) mantle melting anomalies, 2) subduction-related interaction between the Pacific plates and the continental eastern margin, 3) convergent interaction between India and the continental southern margin, and 4) quasiperiodic orbital variations of the Earth. The starting point of the latest geodynamic stage [Rasskazov, Chuvashova, 2013] is consistent with the change of the Earth’s rotation due to the resonant interaction of its orbit with the orbit of the Mars in the time interval of 87–85 Ma [Ma et al., 2017].

At the latest geodynamic stage that is characterized by forces and processes of the last 90 Ma the lithosphere of Asia has been reactivated due to four main force factors: 1) mantle melting anomalies, 2) subduction-related interaction between the Pacific plates and the continental eastern margin, 3) convergent interaction between India and the continental southern margin, and 4) quasiperiodic orbital variations of the Earth. The starting point of the latest geodynamic stage [Rasskazov, Chuvashova, 2013] is consistent with the change of the Earth’s rotation due to the resonant interaction of its orbit with the orbit of the Mars in the time interval of 87–85 Ma [Ma et al., 2017].

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The authors declare that there are no conflicts of interest present.