Мақаланы E-mail арқылы жіберу The Fe2+ occupancies in the silicates M1 and M2 sites in Chelyabinsk LL5 meteorite determined using XRD and Mössbauer spectroscopy
- Авторлар: Maksimova A.A.1, Chukin A.V.1, Semionkin V.A.1, Oshtrakh M.I.1
-
Мекемелер:
- Institute of Physics and Technology
- Шығарылым: Том 81, № 7 (2017)
- Беттер: 845-849
- Бөлім: Article
- URL: https://journals.rcsi.science/1062-8738/article/view/185129
- DOI: https://doi.org/10.3103/S1062873817070188
- ID: 185129
Дәйексөз келтіру
Ашық рұқсат
Рұқсат берілді
Тек жазылушылар үшін
Аннотация
Study of four Chelyabinsk LL5 ordinary chondrite fragments with different lithology was carried out using X-ray diffraction and Mössbauer spectroscopy with a high velocity resolution. The Fe2+ occupancies of the M1 and M2 sites in olivine, orthopyroxene, and clinopyroxene determined using X-ray diffraction and Mössbauer spectroscopy were compared. Distribution coefficients KD and the temperatures of cations equilibrium distribution Teq in the olivine and orthopyroxene were evaluated.
Авторлар туралы
A. Maksimova
Institute of Physics and Technology
Хат алмасуға жауапты Автор.
Email: a.a.maksimova@urfu.ru
Ресей, Yekaterinburg, 620002
A. Chukin
Institute of Physics and Technology
Email: a.a.maksimova@urfu.ru
Ресей, Yekaterinburg, 620002
V. Semionkin
Institute of Physics and Technology
Email: a.a.maksimova@urfu.ru
Ресей, Yekaterinburg, 620002
M. Oshtrakh
Institute of Physics and Technology
Email: a.a.maksimova@urfu.ru
Ресей, Yekaterinburg, 620002
Қосымша файлдар
