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Water transport in natural quartz at high temperaturesтезисы доклада
- Автор: Kreisberg V.A.
- Сборник: Abstracts of the 30th International Geological Congress, 4-14 August, 1996, Beijing, China
- Том: 3
- Тезисы
- Год издания: 1996
- Место издания: The Geological Society of China, Beijing, China
- Первая страница: 22
- Последняя страница: 22
- Аннотация: Diffusion coefficients of water, the main fluid in the earth's crust, in quartz have been determined by mass spectrometry from isothermal kinetic regularities of the intensities of ion current for the evolution of water impurities from quartz grains (fraction 0.1-0.45 mm) of different deposits of Ural region in Russia at temperature range 800-1400 C. Volume diffusion of water through the crystal lattice depeds on defect concentration.
- Добавил в систему: Крейсберг Валерий Абрамович