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В. В. Ревердатто

V.S. Sobolev Institute of Geology and Mineralogy

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И. И. Лиханов

V.S. Sobolev Institute of Geology and Mineralogy

O. P. Polyansky

V.S. Sobolev Institute of Geology and Mineralogy

П. С. Козлов

V.S. Sobolev Institute of Geology and Mineralogy

A. V. Babichev

V.S. Sobolev Institute of Geology and Mineralogy

В. В. Хиллер

Zavaritsky Institute of Geology and Geochemistry

S. N. Korobeynikov

Lavrentyev Institute of Hydrodynamics

A. D. Nozhkin

V.S. Sobolev Institute of Geology and Mineralogy

V Yu Kolobov

V.S. Sobolev Institute of Geology and Mineralogy

V. G. Sverdlova

V.S. Sobolev Institute of Geology and Mineralogy

V. S. Sheplev

V.S. Sobolev Institute of Geology and Mineralogy

Cooperative Institutions

Russian Academy of Sciences

V.S. Sobolev Institute of Geology and Mineralogy

Siberian Branch of the Russian Academy of Sciences

Novosibirsk State University

Institute of the Earth’s Crust

Institute of Mineralogy

Siberian Research Institute of Geology, Geophysics and Mineral Resources

Czech Academy of Sciences, Institute of Geology

Institute of Petroleum Geology and Geophysics

National Research Tomsk State University

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The nature of the heat source of mafic magmatism during the formation of the Vilyui rift based on the ages of dike swarms and results of numerical modeling

Russian Geology and Geophysics (2018)

O. P. Polyansky Andrei V. Prokopiev О. В. Королева М. Д. Томшин В. В. Ревердатто

Dike

Mantle plume

Large igneous province

Flood basalt

Thermal subsidence

10.1016/j.rgg.2018.09.003

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Citations (17)

Three metamorphic events in the precambrian P-T-t history of the Transangarian Yenisey ridge recorded in garnet grains in metapelites

Petrology (2013)

И. И. Лиханов В. В. Ревердатто П. С. Козлов В. В. Хиллер В. П. Сухоруков

Riphean

Orogeny

Geochronology

10.1134/s0869591113060040

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Citations (33)

Zoning of garnets as an indicator of metamorphic evolution in metapelites of the Yenisei Ridge

Doklady Earth Sciences (2014)

И. И. Лиханов В. В. Ревердатто

Grossular

Anorthite

Anorthosite

10.1134/s1028334x14090098

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Citations (7)

Sulfide Mineralization Hosted by Spurrite-Mervinite Marbles (Kochumdek River, East Siberia)

Doklady Earth Sciences (2019)

É. V. Sokol Anna S. Deviatiiarova Svetlana N. Kokh В. В. Ревердатто Dmitry A. Artemyev

10.1134/s1028334x19110163

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Citations (4)

Modelling of the thermal history of metamorphic zoning in the Connemara region (western Ireland)

Tectonophysics (2003)

В. В. Ревердатто O. P. Polyansky

Dalradian

Orogeny

10.1016/j.tecto.2003.10.005

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Citations (10)

Mineral assemblages of the Al2SiO5 “triple point” in metapelites

Doklady Earth Sciences (2013)

И. И. Лиханов В. В. Ревердатто

Triple point

10.1134/s1028334x13010121

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Citations (6)

Mineral Geothermobarometry

Springer geology (2018)

В. В. Ревердатто И. И. Лиханов O. P. Polyansky V. S. Sheplev V Yu Kolobov

Geothermobarometry

TRACE (psycholinguistics)

10.1007/978-3-030-03029-2_2

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Citations (4)

Diffusion‐controlled corona reaction and overstepping of equilibrium in a garnet granulite, Yenisey Ridge, Siberia

Journal of Metamorphic Geology (1998)

J. R. Ashworth V. S. Sheplev N. A. Bryxina V Yu Kolobov В. В. Ревердатто

Diffusion modelling is applied to layered garnet–pyroxene–quartz coronas, formed by a pressure‐induced reaction between plagioclase and primary pyroxene in a metabasic granulite. The reconstructed reaction involves some change in composition of reactant minerals. The distribution of minerals between layers is satisfactorily explained by diffusion‐controlled reaction with local equilibrium, in which the diffusion coefficient for Al was smaller than those for Fe, Mg and Ca by a factor of approximately four. Diffusion of Mg towards plagioclase implies a chemical‐potential gradient for MgO component in a direction opposite to the changing Mg content of garnet; this is explained by the influence of Al 2 O 3 on the chemical potential of the pyrope end‐member. Grain‐boundary diffusion is suggested to have operated, possibly with composition gradients different from those in the bulk minerals. Chemical‐potential differences across the corona are estimated from the variation in garnet composition, enabling affinity (the free energy change driving the reaction) to be estimated as 6.9±1.8 kJ per 24‐oxygen mole of garnet produced. This implies that the pressure for equilibrium among the minerals was overstepped by 1.4±0.4 kbar. The probable P–T conditions of reaction were in the range 650–790 °C, 8–10 kbar. Assuming a timescale of reaction between 10 6 and 10 8 years, estimated diffusion coefficients for Fe, Mg and Ca are in the range 9×10 −23 to 5×10 −20 m 2 s −1 . These are consistent with experimental values in the literature for solid‐state diffusion, including grain‐boundary diffusion.

Pyroxene

10.1111/j.1525-1314.1998.00134.x

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Citations (44)

Contact metamorphism of Fe- and Al-rich graphitic metapelites in the Transangarian region of the Yenisei Ridge, eastern Siberia, Russia

И. И. Лиханов В. В. Ревердатто V. S. Sheplev A.E. Verschinin П. С. Козлов

Andalusite

Geothermobarometry

Cordierite

Sillimanite

Muscovite

Staurolite

Isograd

10.1016/s0024-4937(01)00048-2

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Citations (68)

Characteristics of metasomatism genetically related to hypabyssal basic magmatism

International Geology Review (1973)

A. L. Pavlov В. В. Ревердатто

Metasomatism

10.1080/00206817309476081

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