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Strontium and Neodymium Isotopic Signatures in Basalt Glasses of the Mid-Atlantic Ridge, 12°–31° N.
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- Geochemistry International, 2023, v. 61, n. 12, p. 1241, doi. 10.1134/S0016702923120054
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Variations in the Composition of MORB Chilled Glasses from the Mid-Atlantic Ridge, 12°–31° N: Reflection of Compositional Evolution of Parental Melts and the Influence of a Hydrothermal Component.
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- Petrology, 2023, v. 31, n. 5, p. 475, doi. 10.1134/S0869591123050053
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Carbonation of Serpentinites of the Mid-Atlantic Ridge: 1. Geochemical Trends and Mineral Assemblages.
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- Petrology, 2022, v. 30, p. S25, doi. 10.1134/S0869591123010095
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N–Ar–He–CO<sub>2</sub> Systematics Combined with H<sub>2</sub>O, Cl, K Abundances in MORB Glasses Demonstrate Interaction of Magmatic and Hydrothermal Systems: a Case for MAR at 16°07′–17°11′ N.
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- Geochemistry International, 2022, v. 60, n. 11, p. 1068, doi. 10.1134/S0016702922110027
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Magmatic Complexes of the Stalemate Ridge, Northwest Pacific, and Their Possible Origin.
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- Geochemistry International, 2022, v. 60, n. 5, p. 430, doi. 10.1134/S001670292205010X
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Multiple Melting of a Heterogeneous Mantle and Episodic Accretion of Oceanic Crust in a Spreading Zone: Zircon U-Pb Age and Hf-O Isotope Evidence from an Oceanic Core Complex of the Mid-Atlantic Ridge.
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- Petrology, 2022, v. 30, n. 1, p. 1, doi. 10.1134/S0869591122010040
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Estimating population‐level of alcohol, tobacco and morphine use in a small Russian region using wastewater‐based epidemiology.
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- Drug & Alcohol Review, 2021, v. 40, n. 7, p. 1186, doi. 10.1111/dar.13334
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Amphibolites of the Stalemate Ridge and Shirshov Rise, Northwest Pacific: Indicators of the Geodynamic Regime of Metamorphism at the Convergent Plate Boundary.
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- Geochemistry International, 2021, v. 59, n. 3, p. 213, doi. 10.1134/S0016702921030095
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Mafic–Ultramafic Complexes of the Stalemate Ridge, NW Pacific, and the Shirshov Rise, Bering Sea: Geochemical Similarities and Differences.
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- Petrology, 2021, v. 29, n. 1, p. 1, doi. 10.1134/S0869591121010057
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Influence of the Precipitation Rate on the Isotope (δ18O, δ13C and δ88Sr) Composition of Carbonate Chimneys of the Lost City Hydrothermal Field (30° N, Mid-Atlantic Ridge).
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- Petrology, 2020, v. 28, n. 4, p. 374, doi. 10.1134/S0869591120040037
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U–Pb Dating, Oxygen and Hafnium Isotope Ratios of Zircon from Rocks of Oceanic Core Complexes at the Mid-Atlantic Ridge: Evidence for the Interaction of Contemporary and Ancient Crusts in the Spreading Center of the Ocean Floor.
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- Doklady Earth Sciences, 2019, v. 489, n. 2, p. 1396, doi. 10.1134/S1028334X19120109
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Amphibolites of the Metamorphic Basement of Wrangel Island: Age, Nature of the Protolith, and Conditions of Metamorphism.
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- Geochemistry International, 2019, v. 57, n. 12, p. 1249, doi. 10.1134/S0016702919120103
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Geodynamic Nature of Magmatic Sources in the Northwest Pacific: An Interpretation of Data on the Sr and Nd Isotope Composition of Rocks Dredged at the Stalemate Ridge, Ingenstrem Depression, and Shirshov Rise.
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- Petrology, 2019, v. 27, n. 6, p. 655, doi. 10.1134/S0869591119060079
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Current and Future Trends on Diagnosis and Prognosis of Glioblastoma: From Molecular Biology to Proteomics.
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- Cells (2073-4409), 2019, v. 8, n. 8, p. 863, doi. 10.3390/cells8080863
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Mobility of Dissolved Palladium and Platinum Species during the Water–Rock Interaction in a Chloride Environment: Modeling of PGE Behavior during Interaction between Oceanic Serpentinites and Seawater Derivatives.
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- Geochemistry International, 2019, v. 57, n. 3, p. 282, doi. 10.1134/S0016702919030078
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Ultramafic-Mafic Assemblage of Plutonic Rocks and Hornblende Schists of Shirshov Rise, Bering Sea, and Stalemate Ridge, Northwest Pacific: Geodynamic Interpretations of Geochemical Data.
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- Petrology, 2018, v. 26, n. 5, p. 492, doi. 10.1134/S0869591118050077
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Age of Plutonic Rocks from the Vema Fracture Zone (Central Atlantic) and Nature of Their Mantle Sources.
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- Geochemistry International, 2018, v. 56, n. 2, p. 89, doi. 10.1134/S0016702918020039
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Distribution of siderophile and chalcophile elements in serpentinites of the oceanic lithosphere as an insight into the magmatic and crustal evolution of mantle peridotites.
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- Geochemistry International, 2016, v. 54, n. 12, p. 1019, doi. 10.1134/S0016702916120107
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Petrogenetic conditions at 18°-20° N MAR: Interaction between hydrothermal and magmatic systems.
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- Petrology, 2016, v. 24, n. 4, p. 336, doi. 10.1134/S0869591116040044
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Fluid-rock interaction during seprentinization of oceanic ultramafic rocks hosting the Lost City hydrothermal field, 30° N, MAR.
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- Petrology, 2015, v. 23, n. 6, p. 543, doi. 10.1134/S0869591115050033
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Peridotite-basalt association at MAR between 19°42′ and 19°59′ N: Evaluation of petrogenetic conditions and material balance during hydrothermal transformation of the oceanic crust.
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- Petrology, 2015, v. 23, n. 1, p. 1, doi. 10.1134/S0869591115010051
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Petrology and geochemistry of plutonic rocks in the Northwest Pacific Ocean and their geodynamic interpretation.
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- Geochemistry International, 2014, v. 52, n. 3, p. 179, doi. 10.1134/S0016702914030082
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Geochemical nature and age of the plagiogranite-gabbronorite association of the oceanic core complex of the Mid-Atlantic ridge at 5°10′S.
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- Petrology, 2014, v. 22, n. 2, p. 109, doi. 10.1134/S0869591114020064
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Two-stage evolution of mantle peridotites from the Stalemate Fracture Zone, northwestern Pacific.
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- Geochemistry International, 2013, v. 51, n. 9, p. 683, doi. 10.1134/S0016702913080028
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C, N, He, and Ar isotope and element ratios in fluid inclusions from MORB chilled glasses: Stepwise crushing data.
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- Geochemistry International, 2013, v. 51, n. 4, p. 338, doi. 10.1134/S0016702913020043
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Silicification of peridotites at the stalemate fracture zone (Northwestern Pacific): Reconstruction of the conditions of low-temperature weathering and tectonic interpretation.
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- Petrology, 2012, v. 20, n. 1, p. 21, doi. 10.1134/S0869591112010055
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Hydrothermal systems in peridotites at slow-spreading ridges. Modeling phase transformations and material balance: Role of gabbroids.
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- Petrology, 2011, v. 19, n. 3, p. 217, doi. 10.1134/S0869591111030027
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Peridotite-gabbro-trondhjemite association of the Mid-Atlantic Ridge between 12°58′ and 14°45′N: Ashadze and Logachev hydrothermal vent fields.
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- Geochemistry International, 2011, v. 49, n. 4, p. 323, doi. 10.1134/S0016702911040070
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