Chupin, V P; Vetrin, V R; Rodionov, N V; Matukov, D I; Berezhnaya, N G; Sergeev, S A; Mitrofanov, F P; Smirnov, YuP (2006): Composition of melt inclusions and age of zircons of plagiogneisses from the Kola Superdeep Borehole [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.788243, Supplement to: Chupin, VP et al. (2006): Composition of melt inclusions and age of zircons from plagiogneisses of the Archean complex in the Kola Superdeep Borehole, Baltic Shield. Translated from Doklady Akademii Nauk, Ser. Geol., 2006, 406(4), 533-537, Doklady Earth Sciences, 406(4), 153-157, https://doi.org/10.1134/S1028334X06010363
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Published: 2006 (exact date unknown) • DOI registered: 2012-10-03
Abstract:
A comprehensive study of melt inclusions and SHRIMP dating of zircons from trondhjemite gneisses of the sequence VIII from the Kola Superdeep Borehole has revealed presence of old primary magmatic crystals with age up to 2887+/-15 Ma. This is not consistent with the previous view, according to which the oldest zircons from the Archean Complex in SG-3 are products of granulite metamorphism. Primary magmatic zircons of early generation (from 2887 to 2842 Ma) formed in deep-seated magma chambers during partial crystallization of CO2-saturated trondhjemite estimates on duration of generation of tonalite-trondhjemite-granite melts through partial melting of mafic rocks.
Project(s):
Archive of Ocean Data (ARCOD)
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Latitude: 69.395917 * Longitude: 30.610367
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Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
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2 datasets
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Datasets listed in this publication series
- Chupin, VP; Vetrin, VR; Rodionov, NV et al. (2006): (Table 1) Chemical composition of rock and glasses of heated melt inclusions in zircon of biotite plagiogneisses from the Kola Superdeep Borehole. https://doi.org/10.1594/PANGAEA.788241
- Chupin, VP; Vetrin, VR; Rodionov, NV et al. (2006): (Table 2) U-Pb isotope data on prismatic zircons in biotite plagiogneisses from the Kola Superdeep Borehole. https://doi.org/10.1594/PANGAEA.788242