Experimental calibration of the phlogopite fluorimeter at 500–700 °C and 1–4 kbar, and estimated HF concentrations of fluids associated with marble: Some examples

Author:

Aksyuk A.M.,Zhukovskaya T.N.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference36 articles.

1. The phlogopite skarn deposits: physico-chemical conditions of formation;Aksyuk,1988

2. Peculiarity of regime of H2O and CO2 at regional metamorphism;Aranovich,1987

3. Internally-consistent thermodynamic data for minerals in the system Na2O-K2O-CaO-MgO-FeO-Fe2O3-Al2O3-SiO2-TiO2-H2O-CO2: representation, estimation, and high temperature extrapolation;Berman;J. Petrol.,1988

4. El skarn de W-Sn del Carro del Diablo (Systema Central Español);Casquet;Bol. Geol. Minero,1984

5. Principles of recognition and classification of regional metamorphic formations;Dobretsov;Geol. Geophys.,1969

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