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Internal sources of CO2 during anatexis under conditions of high-temperature metamorphism (experimental data)
Safonov O.G., Khodorevskaya L.I., Kosova S.A., Spivak A.V., Aranovich L.Y.
OXYGEN ISOTOPE SYSTEM OF LEUCOGRANITES OF THE OMSUKCHAN TROUGH (NE RUSSIA): CONDITIONS AND MECHANISMS OF WATER-ROCK INTERACTION
Dubinina Е.О., Filimonova L.G., Avdeenko A.S., Chizhova Y.N., Kossova S.A., Zhilicheva О.М., Aranovich L.Y.
STABILITY OF CARBONATES DURING SUBDUCTION: INFLUENCE OF THE DEHYDRATION REGIME OF CHLORINE-BEARING METAPELITE
Sokol A.G., Kruk A.N., Koz’menko O.A., Palyanov Y.N.
EFFECT OF SULFUR CONCENTRATION ON OLIVINE SULFIDATION UNDER LITHOSPHERIC MANTLE PT-PARAMETERS
Bataleva Y.V., Furman O.V., Zdrokov E.V., Borzdov Y.M., Palyanov Y.N.
Stability of carbonates during subduction: the role of dissolution in dehydration fluids
Kruk A.N., Sokol A.G., Khokhryakov A.F., Palyanov Y.N.
Experimental study of solubility of columbite and pyrochlore, tantalum and niobium oxides in alkaline hydrothermal fluids at 300–550°C, 50 and 100 MPa
Kotova N.P., Korzhinskaya V.S., Shapovalov Y.B.
An estimate of chlorine fugacity in the low water fluid of the system С-О-(Н)-NaCl in the cumulus of ultrabasic-basic intrusions
Simakin A.G., Shaposhnikova O.Y., Devyatova V.N., Isaenko S.I., Eremin D.D.
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