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Showing 1–5 of 5 results
Advanced filters: Author: Michael Bizimis Clear advanced filters

  • Mercury isotopes in Northeast Asia intraplate basalts indicate that the EM1 mantle source contains recycled ancient terrigenous sediments stored in the mantle transition zone for over a billion years, recording long-term deep-Earth volatile cycling.

    • Rong Xu
    • Runsheng Yin
    • Yongsheng Liu
    ResearchOpen Access
    Nature Communications
    Volume: 16, P: 1-10

  • Large igneous provinces may record pulses mantle plume upwellings and their relationship with deep-rooted mantle sources. Madrigal et al. present a new petrological model of the Pacific Ocean Large Igneous Province finding that mantle plume pulses were separated by 10–20 Ma.

    • Pilar Madrigal
    • Esteban Gazel
    • Brian Jicha
    ResearchOpen Access
    Nature Communications
    Volume: 7, P: 1-12

  • Earth’s mantle has cooled since the Archaean. Geochemical identification of anomalously hot lavas formed above the Galapagos Plume 89 million years ago, however, implies that a hot mantle reservoir may have persisted for billions of years.

    • Jarek Trela
    • Esteban Gazel
    • Valentina G. Batanova
    Research
    Nature Geoscience
    Volume: 10, P: 451-456

  • The formation of Bermuda sampled a previously unknown mantle reservoir that is characterized by silica-undersaturated melts enriched in volatiles and by a unique lead isotopic signature, which suggests that the source is young.

    • Sarah E. Mazza
    • Esteban Gazel
    • Alexander V. Sobolev
    Research
    Nature
    Volume: 569, P: 398-403