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200th Anniversary Meeting of the Russian Mineralogical Society
Saint Petersburg, Russia
10-13 October 2017
2017minsoc.ru
http://www.minsoc.ru/2017/
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Conferences & Meetings 200th Anniversary Meeting of the Russian Mineralogical Society
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Thermodynamic model for calculation of Mg3Al2Si3O12 (pyrope) properties and garnet‒ilmenite‒perovskite phase transitions under mantle conditions.

RMS-DPI code:  2017-1-145-0
Scientific session:  4. Minerals as indicators of the rock and ore formation.
Author listing:  Dymshits A.M., Dorogokupets P.I.
Principal author:  Dymshits Anna Mikchailovna
Language:  Russian
Abstract - Summary 
(short description):
Garnets enriched in the pyrope component are found in large amounts in the upper mantle of the Earth and are found in such rocks as peridotites, pyroxenites and eclogites. To date, the pyrope stability field is a very interesting and significant issue for geology, since phase transformations in a simple MgSiO3-MgO system do not adequately describe the boundaries of the transition zone of the Earth\'s upper mantle. Based on a joint analysis of existing experimental measurements, an equation of state of pyrope was constructed. Thermodynamic model was based on the Helmholtz free enegry. The resulting equation of state made it possible to calculate the thermodynamic functions of pyrope as a function of temperature and pressure and to construct a phase diagram.
 
RMS-DPI code:  2017-1-145-0
Pages:  199-201
File of proceedings 
(PDF): 
 151 K
Status:  printed
Recieved:  23/06/2017
Accepted:  16/09/2017
Published on-line:  07/12/2017
Permanent address of publication:  http://www.minsoc.ru/2017-1-145-0/
Contact author(s):  Dymshits, Anna Mikchailovna
 

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