Implications of sepiolite dehydration for earthquake nucleation in the Galera Fault Zone: A thermodynamic approach
A new thermodynamic model for the Mg-phyllosilicate sepiolite was developed and used to calculate its P-T stability conditions and water content for different bulk rock compositions. The standard-state thermodynamic properties, entropy (S°) and enthalpy (H°), were initially estimated by oxide summat...
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Veröffentlicht in: | Applied geochemistry 2018-02, Vol.89, p.219-228 |
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