0183192 - UGN-S 20033061 RIV DE eng J - Journal Article
Zbořil, R. - Mašláň, M. - Barčová, K. - Walla, J. - Ferrow, E. - Martinec, Petr
Thermal behaviour of pyrope at 1000 and 1100 degrees C: mechanism of Fe2+ oxidation and decomposition model.
Physics and Chemistry of Minerals. Roč. 30, - (2003), s. 620-627. ISSN 0342-1791. E-ISSN 1432-2021
R&D Projects: GA ČR GA202/00/0982
Institutional research plan: CEZ:AV0Z3086906
Keywords : Fe-bearing garnet * Mössbauer spectroscopy
Subject RIV: DB - Geology ; Mineralogy
Impact factor: 1.671, year: 2003
DOI: https://doi.org/10.1007/s00269-003-0355-x

Mechanism of thermally induced oxidation of Fe2+ from natural pyrope has been studied at 1000 and 1100 degrees C using 57Fe Mössbauer spectroscopy in conjunction with XRD, XRF, AFM, QELS, TG, DTA and electron microprobe analyses.
Permanent Link: http://hdl.handle.net/11104/0079706