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V. V. Yarmolyuk

Institute of Geology of Ore Deposits Petrography Mineralogy and Geochemistry

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А. М. Kozlovsky

Institute of Geology of Ore Deposits Petrography Mineralogy and Geochemistry

В. И. Коваленко

A.E. Arbuzov Institute of Organic and Physical Chemistry

Е. Б. Сальникова

Institute of Precambrian Geology and Geochronology

В. П. Ковач

Institute of Precambrian Geology and Geochronology

E. A. Kudryashova

Institute of Geology of Ore Deposits Petrography Mineralogy and Geochemistry

В. М. Саватенков

Institute of Precambrian Geology and Geochronology

A. B. Kotov

Institute of Precambrian Geology and Geochronology

M. I. Kuzmin

Vinogradov Institute of Geochemistry

А. В. Никифоров

Institute of Geology of Ore Deposits Petrography Mineralogy and Geochemistry

A. A. Vorontsov

Vinogradov Institute of Geochemistry

Cooperative Institutions

Russian Academy of Sciences

Institute of Geology of Ore Deposits Petrography Mineralogy and Geochemistry

Institute of Precambrian Geology and Geochronology

Vinogradov Institute of Geochemistry

Institute of the Earth’s Crust

Siberian Branch of the Russian Academy of Sciences

Geological Institute

V.I. Vernadsky Institute of Geochemistry and Analytical Chemistry

V.S. Sobolev Institute of Geology and Mineralogy

Czech Academy of Sciences, Institute of Geology

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Intraplate geodynamics and magmatism in the evolution of the Central Asian Orogenic Belt

Journal of Asian Earth Sciences (2014)

V. V. Yarmolyuk M. I. Kuzmin Richard E. Ernst

Mantle plume

Rodinia

Supercontinent

10.1016/j.jseaes.2014.07.004

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Citations (95)

Contribution of alkaline granite magmatism to the formation of the Khangai batholith: Geological and geochronological evidence

Doklady Earth Sciences (2013)

V. V. Yarmolyuk А. М. Kozlovsky Е. Б. Сальникова A. B. Kotov А. В. Травин

Batholith

10.1134/s1028334x13100127

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Citations (8)

Microcontinents among the accretionary complexes of the Central Asia Orogenic Belt: In situ Re–Os evidence

Journal of Asian Earth Sciences (2011)

Kuo‐Lung Wang Suzanne Y. O′Reilly В. П. Ковач William L. Griffin Norman J. Pearson

Peridotite

10.1016/j.jseaes.2011.09.016

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Citations (15)

Timing of accretion of the Malkhan-Konda Terrane (Western Transbaikal Region) to the Siberian Paleocontinent: Results of U-Pb geochronological studies of the granitoids of the Malkhan Complex

Doklady Earth Sciences (2013)

E. Yu. Rytsk Е. Б. Сальникова В. П. Ковач A. B. Kotov V. V. Yarmolyuk

10.1134/s1028334x13010200

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Citations (4)

The evolution of volcanism in the Tugnui-Khilok sector of the western Transbaikalia rift area in the Late Mesozoic and Cenozoic

Journal of Volcanology and Seismology (2007)

A. A. Vorontsov V. V. Yarmolyuk

Radiogenic nuclide

10.1134/s074204630704001x

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Citations (18)

Tholeiitic and Alkaline Basaltic Lavas of Wang-Tian’e and Changbaishan Volcanoes (Northeastern China): Timing and Genetic Relationship

Doklady Earth Sciences (2022)

О. А. Андреева V. V. Yarmolyuk В. М. Саватенков I. A. Andreeva V. А. Lebedev

Flood basalt

Tian

10.1134/s1028334x22600323

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Citations (3)

Geodynamic Environments of the Origin of Poly- and Monometamorphic Complexes in the Southern Altai Metamorphic Belt, Central Asian Orogenic Belt

Petrology (2019)

И. К. Козаков А. М. Kozlovsky V. V. Yarmolyuk T. I. Kirnozova M. M. Fugzan

Protolith

Sillimanite

Massif

Anatexis

10.1134/s0869591119030032

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Citations (13)

Precambrian terrains of Central Asian orogenic belt: comparative characteristics, types and peculiarities of the tectonic evolution

Геотектоника (2019)

V. V. Yarmolyuk К. Е. Degtyarev

Supercontinent

Rodinia

Orogeny

10.31857/s0016-853x201913-43

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Citations (3)

Mechanism of carbonate assimilation by intraplate basaltic magma and liquid immiscibility: example of Wangtian’e volcano (Changbaishan volcanic area, NE China)

Frontiers in Earth Science (2023)

О. А. Андреева Е. О. Дубинина Irina A. Andreeva V. V. Yarmolyuk A. Yu. Bychkov

The balance of CO 2 during abundant basaltic magma production is an important factor of volcanic hazards and climate. In particular, this can be explored based on CO 2 -rich mantle-derived magmas or carbonate assimilation by basaltic melts. To reconstruct the origin of Fe-rich carbonates hosted by Cenozoic basalts from Wangtian’e volcano (northeast China), we studied elemental compositions of melt, crystalline and fluid inclusions in magmatic minerals as well as the oxygen and carbon isotope compositions of the plagioclase and carbonates from basalts. The crystallization of basaltic magmas occurred in shallow chamber (∼4 km) at temperatures of 1,180°C–1,200°C and a pressure of 0.1 ± 0.01 GPa. Stable Fe-rich carbonates occur in the Wangtian’e tholeiite basalts as groundmass minerals, crystalline inclusions in plagioclase and globules in melt inclusions, which suggests that they crystallized from a ferrocarbonate melt. The values of δ 18 О and δ 13 С in the minerals analyzed by laser fluorination method are in line with the sedimentary source of Fe-rich carbonates, indicating assimilation and partial decomposition of carbonate phases. The parent ferrocarbonate melt could be produced during interactions between the basaltic magma and the crustal marbles. The phase diagram and thermodynamic calculations show that the ferrocarbonate melt is stable at a temperature of 1,200°C and a pressure of 0.1 GPa. Our thermodynamic calculations show that carbonate melt containing 73 wt% FeCO 3 , 24 wt% MgCO 3 and 3 wt% CaCO 3 is in thermodynamic equilibrium with silicate melt in agreement with our natural observations. The proposed mechanism is crustal carbonate sediment assimilation by the intraplate basaltic magma resulting in the melt immiscibility, production of the ferrocarbonate melt and the following Fe-rich carbonate mineral crystallization during magma residence and cooling.

Melt inclusions

Carbonate minerals

10.3389/feart.2023.1306460

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Citations (2)

Contrasting origin of two A-type rhyolite series from the Early Permian Nomgon bimodal volcanic association (Southern Mongolia)

Doklady Earth Sciences (2017)

А. М. Kozlovsky V. V. Yarmolyuk В. М. Саватенков E. A. Kudryashova

Anatexis

Volcanic plateau

10.1134/s1028334x17080141

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