Ultrahigh-Pressure Liquation of an Impact Melt
- 作者: 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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隶属关系:
- Institute of Geology, Komi Science Center, Ural Branch
- Hawaii Institute of Geophysics and Planetology
- 期: 卷 480, 编号 1 (2018)
- 页面: 595-598
- 栏目: Geochemistry
- URL: https://journals.rcsi.science/1028-334X/article/view/193072
- DOI: https://doi.org/10.1134/S1028334X18050070
- ID: 193072
如何引用文章
详细
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.
作者简介
T. Shumilova
Institute of Geology, Komi Science Center, Ural Branch; Hawaii Institute of Geophysics and Planetology
编辑信件的主要联系方式.
Email: shumilova@geo.komisc.ru
俄罗斯联邦, Syktyvkar; Honolulu
S. Isaenko
Institute of Geology, Komi Science Center, Ural Branch
Email: shumilova@geo.komisc.ru
俄罗斯联邦, Syktyvkar
B. Makeev
Institute of Geology, Komi Science Center, Ural Branch
Email: shumilova@geo.komisc.ru
俄罗斯联邦, Syktyvkar
A. Zubov
Institute of Geology, Komi Science Center, Ural Branch
Email: shumilova@geo.komisc.ru
俄罗斯联邦, Syktyvkar
S. Shanina
Institute of Geology, Komi Science Center, Ural Branch
Email: shumilova@geo.komisc.ru
俄罗斯联邦, Syktyvkar
Ye. Tropnikov
Institute of Geology, Komi Science Center, Ural Branch
Email: shumilova@geo.komisc.ru
俄罗斯联邦, Syktyvkar
A. Askhabov
Institute of Geology, Komi Science Center, Ural Branch
Email: shumilova@geo.komisc.ru
俄罗斯联邦, Syktyvkar