MG-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 PROTOLITHS
https://doi.org/10.5800/GT-2017-8-3-0283
Аннотация
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.
Об авторах
A. V. Pilitsyna
Geological Institute of RAS
Россия
Moscow
Россия
Moscow
A. A. Tretyakov
Geological Institute of RAS
Россия
Moscow
Россия
Moscow
T. A. Alifirova
V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of RAS
Россия
Novosibirsk
Россия
Novosibirsk
K. E. Degtyarev
Geological Institute of RAS
Россия
Moscow
Россия
Moscow
Список литературы
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Рецензия
Для цитирования:
Pilitsyna A.V., Tretyakov A.A., Alifirova T.A., Degtyarev K.E. MG-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 PROTOLITHS. Геодинамика и тектонофизика. 2017;8(3):533-536. https://doi.org/10.5800/GT-2017-8-3-0283
For citation:
Pilitsyna A.V., Tretyakov A.A., Alifirova T.A., Degtyarev K.E. MG-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 PROTOLITHS. Geodynamics & Tectonophysics. 2017;8(3):533-536. https://doi.org/10.5800/GT-2017-8-3-0283
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