Oxygen isotopic composition of coexisting minerals of sillimanite-hypersthene rocks from the Por’ya bay area: Evidence of fluid involvement in granulite-facies metamorphism

Author:

Aranovich L. Ya.,Dubinina E. O.,Avdeenko A. S.,Lebedeva Yu. M.,Bushmin S. A.,Dolivo-Dobrovol’skii D. D.

Publisher

Pleiades Publishing Ltd

Subject

Geochemistry and Petrology,Geophysics

Reference27 articles.

1. W. S. Fyfe, “The Granulite Facies, Partial Melting and the Archean Crust,” Phil. Trans. R. Soc. London 273, 457–461 (1973).

2. A. B. Thompson, “Dehydration Melting of Pelitic Rocks and the Generation of H2O-Undersaturated Liquids,” Am. J. Sci. 282, 1567–1595 (1982).

3. L. Ya. Aranovich, K. I. Shmulovich, and V. V. Fed’kin, “H2O and CO2 Regime at Regional Metamorphism,” In Contributions to Physicochemical Petrology, Ed. by V. A. Zharikov (Nauka, Moscow, 1987), pp. 96–117 [in Russian].

4. R. C. Newton, L. Y. Aranovich, E. C. Hansen, and B. A. Vandenheuvel, “Hypersaline Fluids in Precambrian Deep-Crustal Metamorphism,” Precambrian Res. 38, 21–34 (1998).

5. R. Nair and T. Chacko, “Fluid-Absent Melting of High-Grade Semi-Pelites: P-T Constraints on Orthopyroxene Formation and Implications for Granulite Genesis,” J. Petrol. 43, 2121–2143 (2002).

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