gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2017-8-3-0283gtcrust-424Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSMG-CR-TYPE SPINEL PERIDOTITES IN THE WESTERN PART OF THE CENTRAL ASIAN OROGENIC BELT (ZHELTAU MASSIF, SOUTHERN KAZAKHSTAN): THE FIRST DATA ON P-T PATHS AND PROTOLITHSMG-CR-TYPE SPINEL PERIDOTITES IN THE WESTERN PART OF THE CENTRAL ASIAN OROGENIC BELT (ZHELTAU MASSIF, SOUTHERN KAZAKHSTAN): THE FIRST DATA ON P-T PATHS AND PROTOLITHSPilitsynaA. V.PilitsynaA. V.

Moscow

Moscow

TretyakovA. A.TretyakovA. A.

Moscow

Moscow

AlifirovaT. A.AlifirovaT. A.

Novosibirsk

Novosibirsk

DegtyarevK. E.DegtyarevK. E.

Moscow

Moscow

Geological Institute of RASРоссияGeological Institute of RASRussian FederationV.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of RASРоссияV.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of RASRussian Federation20171210201783533536Copyright © Pilitsyna A.V., Tretyakov A.A., Alifirova T.A., Degtyarev K.E., 20172017Pilitsyna A.V., Tretyakov A.A., Alifirova T.A., Degtyarev K.E.Pilitsyna A.V., Tretyakov A.A., Alifirova T.A., Degtyarev K.E.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/424

Ultramafic and mafic lithologies, attributed to the orogenic terranes and formed under ultrahigh-pressure (UHP) and high-pressure (HP) conditions, have been intensively studied for the last decades. It is mainly related to a particular significance of these rocks for geodynamics, since they contain an important information on the fluid-rock interactions and element redistribution in the subduction-collision zones and could shed the light on the tectonic evolution of the studied region.

Ultramafic and mafic lithologies, attributed to the orogenic terranes and formed under ultrahigh-pressure (UHP) and high-pressure (HP) conditions, have been intensively studied for the last decades. It is mainly related to a particular significance of these rocks for geodynamics, since they contain an important information on the fluid-rock interactions and element redistribution in the subduction-collision zones and could shed the light on the tectonic evolution of the studied region.

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