Английская Википедия:Angara-Vitim batholith

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Версия от 21:42, 31 января 2024; EducationBot (обсуждение | вклад) (Новая страница: «{{Английская Википедия/Панель перехода}} The '''Angara-Vitim batholith''' is group of plutons in the eastern Siberia, just east of Lake Baikal. The batholith formed in the DevonianEarly Carboniferous likely in connection to a mantle plume. It formed about the same time and by the same process as the Kalba-Narym batholith in eastern Kazakhstan.<ref name=Khroetal2016>{{cite journal |last1=Khromykh...»)
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The Angara-Vitim batholith is group of plutons in the eastern Siberia, just east of Lake Baikal. The batholith formed in the DevonianEarly Carboniferous likely in connection to a mantle plume. It formed about the same time and by the same process as the Kalba-Narym batholith in eastern Kazakhstan.[1]

Common rock types are granite with biotite and granodiorite. The rocks belong to the high-K and shoshonite subseries of the calc-alkaline magma series. Some rocks do belong to the alkaline magma series.[1]

References

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