P-T-fluid regimes of metamorphism and related magmatism with specific reference to the granulite-facies Sharyzhalgay complex of Lake Baikal

Author:

Perchuk Leonid L.

Publisher

Geological Society of London

Subject

Geology,Ocean Engineering,Water Science and Technology

Reference51 articles.

1. Abramovich I. I. Klushin I. G. (1978) Petrochemistry and Structure of Earth Interiors (Nedra Press, Leningrad) (in Russian). 370.

2. Biotite-garnet equilibria in metapelites. 1. Thermodynamics of solid solutions and mineral reactions;Aranovich;Contributions to Physicochemical Petrology,1983

3. Equilibrium cordierite = orthopyroxene + quartz: experimental data and thermodynamics of ternary Fe-Mg-Al orthopyroxene solid solution;Aranovich;Geochimiya,1986

4. Aranovich L. Ya. Podlesskii K. K. (1983) in Kinetics and Equilibrium in Mineral Reactions, Advances in Physical Geochemistry, The cordierite-garnet-sillimanite-quartz equilibrium: experiments and applications, ed Saxena S. K. (Springer-Verlag, New York), pp 173–198.

5. Development of P-T prograde and P-retrograde, T-prograde isogradic surfaces during blueschist to eclogite regional deformation/metamorphism in New Caledonia, as indicated by progressively developed porphyroblast microstructures;Bell;Journal of Metamorphic Geology,1985

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