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The Magmatic-Hydrothermal Transition and Origin of Brine in the Oceanic Core Complex of the Mid-Atlantic Ridge at 13° N.
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- Doklady Earth Sciences, 2018, v. 480, n. 1, p. 661, doi. 10.1134/S1028334X18050288
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New chemical and isotopic data for basalts from the axial segment of the Mid-Atlantic ridge between the Vema and Mercury fracture zones.
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- Doklady Earth Sciences, 2014, v. 459, n. 2, p. 1488, doi. 10.1134/S1028334X14120137
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Peculiarities of present-day sulfide mineralization at 19°15′-20°08′ N, Mid-Atlantic Ridge.
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- Doklady Earth Sciences, 2012, v. 442, n. 2, p. 163, doi. 10.1134/S1028334X1202002X
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Small-Scale Reactional Features in Abyssal Peridotites from the Mid-Atlantic Ridge at 17°04′ to 17°10′ N.
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- Petrology, 2020, v. 28, n. 4, p. 389, doi. 10.1134/S0869591120040062
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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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- Article