Oxygen isotopic composition of coexisting minerals of sillimanite-hypersthene rocks from the Por'ya Bay area: Evidence of fluid involvement in granulite-fades metamorphism.
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dc.contributor.author | Aranovich, L Ya | |
dc.contributor.author | Dubinina, E O | |
dc.contributor.author | Avdeenko, A S | |
dc.contributor.author | Lebedeva, YuM | |
dc.contributor.author | Bushmin, S A | |
dc.contributor.author | Dolivo-Dobrovol'skii, D D | |
dc.coverage.spatial | MEDIAN LATITUDE: 66.679414 * MEDIAN LONGITUDE: 33.865200 * SOUTH-BOUND LATITUDE: 66.677600 * WEST-BOUND LONGITUDE: 33.863900 * NORTH-BOUND LATITUDE: 66.680200 * EAST-BOUND LONGITUDE: 33.867900 | |
dc.date.accessioned | 2019-11-13T06:20:16Z | |
dc.date.available | 2019-11-13T06:20:16Z | |
dc.date.issued | 2010-08-03 | |
dc.identifier | https://doi.pangaea.de/10.1594/PANGAEA.786970 | |
dc.identifier | https://doi.org/10.1594/PANGAEA.786970 | |
dc.identifier.citation | Aranovich, L Ya; Dubinina, E O; Avdeenko, A S; Lebedeva, YuM; Bushmin, S A; Dolivo-Dobrovol'skii, D D (2010): Oxygen isotopic composition of coexisting minerals of sillimanite-hypersthene rocks from the Por'ya Bay area: Evidence of fluid involvement in granulite-fades metamorphism. Translated from Geokhimiya, 2010, 48(8), 787-800, Geochemistry International, 48(8), 739-751, https://doi.org/10.1134/S001670291008001X | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/6595 | |
dc.format | text/tab-separated-values, 49 data points | |
dc.language.iso | en | |
dc.publisher | PANGAEA | |
dc.relation.isbasedon | Aranovich, L Ya; Dubinina, E O; Avdeenko, A S; Lebedeva, YuM; Bushmin, S A; Dolivo-Dobrovol'skii, D D (2010): Oxygen isotopic composition of coexisting minerals of sillimanite-hypersthene rocks from the Por'ya Bay area: Evidence of fluid involvement in granulite-fades metamorphism. Translated from Geokhimiya, 2010, 48(8), 787-800, Geochemistry International, 48(8), 739-751, https://doi.org/10.1134/S001670291008001X | |
dc.relation.uri | https://doi.org/10.1594/PANGAEA.786975 | |
dc.rights | CC-BY-3.0: Creative Commons Attribution 3.0 Unported | |
dc.rights | Access constraints: unrestricted | |
dc.subject | Archive of Ocean Data | |
dc.subject | ARCOD | |
dc.subject | B1016-21 | |
dc.subject | B1016-24 | |
dc.subject | L4-1 | |
dc.subject | L4-1a | |
dc.subject | L4-2 | |
dc.subject | L4-3 | |
dc.subject | L4-6 | |
dc.subject | Mineral assemblage | |
dc.subject | OUTCROP | |
dc.subject | Outcrop sample | |
dc.subject | Oxygen | |
dc.subject | Palenyi Island, White Sea | |
dc.subject | Rock type | |
dc.subject | Wet chemistry | |
dc.title | Oxygen isotopic composition of coexisting minerals of sillimanite-hypersthene rocks from the Por'ya Bay area: Evidence of fluid involvement in granulite-fades metamorphism. | |
dc.title.alternative | (Table 2) Brief characteristics of samples from the Palenyi Island and oxygen mole fractions corresponding to major rock-forming minerals | |
dc.type | Dataset |
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