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- W4285403234 abstract "Peridotite clasts in a marine Miocene conglomerate from the Torino Hill (NW Italy) are characterised by an isopachous serpentinized external rim (4–12 mm thick) made up of lizardite, surrounding a non-serpentinized peridotite core. This peculiar structure indicates a diagenetic, post-depositional serpentinization of the peridotite clasts. The conglomerate is cemented by a rim of lizardite, followed by Mg-calcite and Ca-dolomite spar. The burial history of the host sedimentary succession indicates that serpentinization and precipitation of lizardite cements probably occurred at very low temperature (max. 50–60 °C). This is the first reported case of diagenetic, very low temperature serpentinization affecting ultramafite clasts in sedimentary successions. • Peridotite pebbles/cobbles with serpentinized rim (lizardite) in a Miocene conglomerate. • Conglomerate is cemented by lizardite rims, followed by Mg-rich carbonates. • Rim serpentinization is post-depositional. • Geological evolution indicates a maximum burial depth of 1500 m, corresponding to 50–60 °C. • Low-temperature, diagenetic serpentinization of peridotite clasts." @default.
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- W4285403234 date "2022-09-01" @default.
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- W4285403234 title "Low-temperature, diagenetic serpentinization of peridotite clasts in lower Miocene marine conglomerates, Torino Hill, NW Italy" @default.
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- W4285403234 doi "https://doi.org/10.1016/j.marpetgeo.2022.105830" @default.
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