@article{fdi:010067897,
  title = {{S}ynthesis of magnesite at low temperature},
  author = {dos {A}njos, {A}. {P}. {A}. and {S}ifeddine, {A}bdelfettah and {S}anders, {C}. {J}. and {P}atchineelam, {S}. {R}.},
  editor = {},
  language = {{ENG}},
  abstract = {{M}agnesite formed at relatively low temperatures, 40{A} degrees {C}, and atmospheric pressure using the experimental duplications is described in {D}eelman (1999). {T}he original experiment itself is a variation of {L}iebermann's (1967) experiments on dolomite formation. {T}he initial products of the reaction were metastable carbonates, aragonite and dypingite which will change during the course of the experiment into magnesite. {T}his 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.},
  keywords = {{M}agnesite ; {L}ow-temperature synthesis},
  booktitle = {},
  journal = {{C}arbonates and {E}vaporites},
  volume = {26},
  numero = {3},
  pages = {213--215},
  ISSN = {0891-2556},
  year = {2011},
  DOI = {10.1007/s13146-011-0063-4},
  URL = {https://www.documentation.ird.fr/hor/fdi:010067897},
}