Инд. авторы: Dobretsov N.L., Chepurov A.I., Sonin V.M., Zhimulev E.I.
Заглавие: Stability of Zircon in the System MgO-SiO2-H2O at 2.5 GPa
Библ. ссылка: Dobretsov N.L., Chepurov A.I., Sonin V.M., Zhimulev E.I. Stability of Zircon in the System MgO-SiO2-H2O at 2.5 GPa // Russian Geology and Geophysics. - 2019. - Vol.60. - Iss. 4. - P.447-450. - ISSN 1068-7971. - EISSN 1878-030X.
Внешние системы: DOI: 10.15372/RGG2019043; РИНЦ: 38693732; SCOPUS: 2-s2.0-85064979513; WoS: 000465259800006;
Реферат: eng: We report preliminary experimental data on the interaction of zircon with the peridotitic assemblage olivine + serpentine at 2.5 GPa and 1400 degrees C. In these conditions, zircon is unstable and decomposes with the formation of baddeleyite. Therefore, it is unlikely that zircon could survive in ultramafic rocks for a long time in the presence of a fluid phase at high temperatures. Thus, rigorous constraints on boundary conditions are required for the use of zircon in the dating of high-temperature geologic processes.
Ключевые слова: PROTOLITH; SOLUBILITY; TEMPERATURES; MINERALS; AQUEOUS FLUIDS; CHINA; high pressure; peridotitic mineral assemblage; baddeleyite; zircon; high temperature; CARBONATE;
Издано: 2019
Физ. характеристика: с.447-450