Mineral Composition and Structure of the Sverdlovsk Meteorite (H4-5)
- Авторлар: Berzin S.1, Koroteev V.1, Ivanov K.1, Kleimenov D.1, Kiseleva D.1, Cherednichenko N.1
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Мекемелер:
- Zavaritsky Institute of Geology and Geochemistry, Ural Branch
- Шығарылым: Том 479, № 1 (2018)
- Беттер: 390-392
- Бөлім: Geochemistry
- URL: https://journals.rcsi.science/1028-334X/article/view/192561
- DOI: https://doi.org/10.1134/S1028334X18030248
- ID: 192561
Дәйексөз келтіру
Аннотация
A fragment of the Sverdlovsk Meteorite, which was found in 1985 in the Central Urals, is studied by modern analytical methods. It belongs to H chondrites of petrologic type 4–5; shock stage of meteorite is S1-2, terrestrial weathering is W1. The composition of minerals of the meteorite is studied. It is found for the first time that the metal and sulfides are concentrated in fine veinlets of the recrystallized matrix of the chondrite and are accompanied by segregations of metal and troilite inside these veinlets. The distribution of trace elements of the metal phase of the meteorite is studied.
Авторлар туралы
S. Berzin
Zavaritsky Institute of Geology and Geochemistry, Ural Branch
Хат алмасуға жауапты Автор.
Email: sbersin@yandex.ru
Ресей, Yekaterinburg, 620016
V. Koroteev
Zavaritsky Institute of Geology and Geochemistry, Ural Branch
Email: sbersin@yandex.ru
Ресей, Yekaterinburg, 620016
K. Ivanov
Zavaritsky Institute of Geology and Geochemistry, Ural Branch
Email: sbersin@yandex.ru
Ресей, Yekaterinburg, 620016
D. Kleimenov
Zavaritsky Institute of Geology and Geochemistry, Ural Branch
Email: sbersin@yandex.ru
Ресей, Yekaterinburg, 620016
D. Kiseleva
Zavaritsky Institute of Geology and Geochemistry, Ural Branch
Email: sbersin@yandex.ru
Ресей, Yekaterinburg, 620016
N. Cherednichenko
Zavaritsky Institute of Geology and Geochemistry, Ural Branch
Email: sbersin@yandex.ru
Ресей, Yekaterinburg, 620016