dos Anjos A. P. A. auteur aut IRD Sifeddine Abdelfettah auteur aut IRD Sanders C. J. auteur aut IRD Patchineelam S. R. auteur aut IRD text journalArticle eng text/pdf born digital access Magnesite formed at relatively low temperatures, 40A degrees C, and atmospheric pressure using the experimental duplications is described in Deelman (1999). The original experiment itself is a variation of Liebermann's (1967) experiments on dolomite formation. The initial products of the reaction were metastable carbonates, aragonite and dypingite which will change during the course of the experiment into magnesite. This work reports to have found evidence in support of an active role of alternations between precipitation and dissolution in bringing about a formation of the thermodynamically stable phase in the magnesite formation. specialized Magnesite Low-temperature synthesis 064 26 3 213-215 2011 0891-2556 https://www.documentation.ird.fr/hor/PAR00008071 10.1007/s13146-011-0063-4 0891-2556 [F B010067897] https://www.documentation.ird.fr/hor/PAR00008071 https://www.documentation.ird.fr/intranet/publi/depot/2016-08-17/010067897.pdf Accès réservé (Intranet de l'IRD) IRD - Base Horizon / Pleins textes 2011-11-30 2017-08-23 PAR00008071 fre