In situ observation of chrysotile decomposition in the presence of NaCl-bearing aqueous fluid up to 5 GPa and 400 °C

Author:

Likhacheva Anna Yu.ORCID,Goryainov Sergey V.,Rashchenko Sergey V.,Dementiev Sergey N.,Safonov Oleg G.

Funder

RFBR

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference42 articles.

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2. Aranovich LY, Newton RC (1997) H2O activity in concentrated KCl and KCl-NaCl solutions at high temperatures and pressures measured by the brucite-periclase equilibrium. Contrib Mineral Petrol 127:261–271

3. Auzende A-L, Daniel I, Reynard B, Lemaire C, Guyot F (2004) High-pressure behavior of serpentine minerals: a Raman spectroscopic study. Am Mineral 31:269–277

4. Chernosky JV Jr, Berman RG, Bryndzia LT (1988) Serpentine and chlorite equilibria. In: Bailey SW (ed) Hydrous phyllosilicates other than micas, vol 19. Mineralogical Society of America, reviews in mineralogy, V, pp 295–346

5. Chligui M, Guimbretiere G, Canizares A, Matzen G, Vaills Y (2010) New features in the Raman spectrum of silica: key-points in the improvement on structure knowledge. 2010. https://hal.archives-ouvertes.fr/hal-00520823/

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