Ultrahigh-Pressure Liquation of an Impact Melt
- Авторы: Shumilova T.1,2, Isaenko S.1, Makeev B.1, Zubov A.1, Shanina S.1, Tropnikov Y.1, Askhabov A.1
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Учреждения:
- Institute of Geology, Komi Science Center, Ural Branch
- Hawaii Institute of Geophysics and Planetology
- Выпуск: Том 480, № 1 (2018)
- Страницы: 595-598
- Раздел: Geochemistry
- URL: https://journals.rcsi.science/1028-334X/article/view/193072
- DOI: https://doi.org/10.1134/S1028334X18050070
- ID: 193072
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Аннотация
Liquation structures were described in ultrahigh-pressure impact glasses of the Kara astrobleme (Pay-Khoy) with differentiation into the bisilica, aluminosilicate, and ore components for the first time. The sequence of differentiation of mineral phases upon solidification of an ultrahigh-pressure impact melt was established: coesite, silicate glass, augite, aluminosilicate glass of albite composition, and pyrite. The discovered impact glasses are highly resistant to postimpact alterations.
Об авторах
T. Shumilova
Institute of Geology, Komi Science Center, Ural Branch; Hawaii Institute of Geophysics and Planetology
Автор, ответственный за переписку.
Email: shumilova@geo.komisc.ru
Россия, Syktyvkar; Honolulu
S. Isaenko
Institute of Geology, Komi Science Center, Ural Branch
Email: shumilova@geo.komisc.ru
Россия, Syktyvkar
B. Makeev
Institute of Geology, Komi Science Center, Ural Branch
Email: shumilova@geo.komisc.ru
Россия, Syktyvkar
A. Zubov
Institute of Geology, Komi Science Center, Ural Branch
Email: shumilova@geo.komisc.ru
Россия, Syktyvkar
S. Shanina
Institute of Geology, Komi Science Center, Ural Branch
Email: shumilova@geo.komisc.ru
Россия, Syktyvkar
Ye. Tropnikov
Institute of Geology, Komi Science Center, Ural Branch
Email: shumilova@geo.komisc.ru
Россия, Syktyvkar
A. Askhabov
Institute of Geology, Komi Science Center, Ural Branch
Email: shumilova@geo.komisc.ru
Россия, Syktyvkar