Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Nikolay V. Bryanskiy"'
Autor:
Anas A. Karimov, Marina A. Gornova, Vasiliy A. Belyaev, Sergei Yu. Skuzovatov, Alexander Ya. Medvedev, Nikolay V. Bryanskiy
Publikováno v:
Minerals, Vol 14, Iss 5, p 457 (2024)
In order to assess the geochemical effects of retrograde metamorphic rehydration, fluid metasomatism, and the fluid-mobile elements (FMEs) budget in the case of oceanic and continental subduction, we report the petrography, bulk, and in situ LA-ICP-M
Externí odkaz:
https://doaj.org/article/766b7fbc10894850ade28419ca76df7a
Autor:
Marina A. Gornova, Vasiliy A. Belyaev, Anas A. Karimov, Sergei Yu. Skuzovatov, Nikolay S. Karmanov, Alexander Ya. Medvedev, Nikolay V. Bryanskiy
Publikováno v:
Frontiers in Earth Science, Vol 11 (2023)
Mantle peridotites from the Mesoproterozoic forearc-type ophiolites in the Eastern Sayan range (Eastern Siberia) provide insights into the nature and formation processes of the supra-subduction mantle. The peridotites are represented by porphyroclast
Externí odkaz:
https://doaj.org/article/dbcf4d32bcc1412eade35b04f8e412bd
Autor:
Anas A. Karimov, Marina A. Gornova, Vasiliy A. Belyaev, Aleksander Ya. Medvedev, Nikolay V. Bryanskiy
Publikováno v:
China Geology, Vol 3, Iss 2, Pp 299-313 (2020)
ABSTRACT: Swarms of orthopyroxenite and websterite veins are found within Egiingol residual SSZ peridotite massif of Dzhida terrain (Central Asian Orogenic Belt, Northern Mongolia). The process of Egiingol pyroxenite veins formation is investigated u
Externí odkaz:
https://doaj.org/article/78f45ecbc0ba44f383db7e1b45e339f1
Publikováno v:
China Geology. 3:299-313
Swarms of orthopyroxenite and websterite veins are found within Egiingol residual SSZ peridotite massif of Dzhida terrain (Central Asian Orogenic Belt, Northern Mongolia). The process of Egiingol pyroxenite veins formation is investigated using new m
Autor:
Richard E. Ernst, Olga Yu. Belozerova, Vadim S. Kamenetsky, Oleg M. Glazunov, Alexei V. Ivanov, Nikolay V. Bryanskiy, Tamara Yu. Yakich, Alexander E. Marfin, Maya B. Kamenetsky, Sandra L. Kamo, I. F. Gertner, Tatiana A. Radomskaya
Publikováno v:
Journal of Petrology. 62
The initial stage of Rodinia supercontinent break-up occurred at about 750 Ma. It preceded formation of the Irkutsk and Franklin large igneous provinces (LIPs) at 712 ± 2 to 739 ± 8 Ma. These LIPs were emplaced within the formerly connected Laurent