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Showing 1–4 of 4 results
Advanced filters: Author: M. Paulatto Clear advanced filters

  • During subduction water is transported into the mantle, but constraining its release remains challenging. Here, using seismic tomography of the Lesser Antilles arc, the authors track the multistage dehydration of the slab and its lateral variations associated with heterogeneous slab composition.

    • Michele Paulatto
    • Mireille Laigle
    • Heidrun Kopp
    ResearchOpen Access
    Nature Communications
    Volume: 8, P: 1-11

  • The vast majority of Earth’s volcanoes are under water, but little is known of the structure and evolution of submarine volcanoes. A bathymetric survey mapping the Monowai submarine volcano in the Tonga–Kermadec Arc twice within 14 days reveals dramatic changes in bathymetry of up to 71.9 m, associated with volcanic activity.

    • A. B. Watts
    • C. Peirce
    • C. E. J. de Ronde
    Research
    Nature Geoscience
    Volume: 5, P: 510-515

  • Raman spectroscopy has become an invaluable tool for graphene characterisation, yet the nature of the broadening of the Raman 2D line remains unclear. Here, Stampferet al. show that the Raman 2D line width is a measure of nanometre-scale strain variations in graphene on insulating substrates.

    • C. Neumann
    • S. Reichardt
    • C. Stampfer
    ResearchOpen Access
    Nature Communications
    Volume: 6, P: 1-7

  • The Bronze Age eruption of Santorini is known to have generated tsunamis with caldera collapse as the likely mechanism. However, new bathymetric and seismic data presented by Nomikou et al. show that the entry of pyroclastic flows into the sea is the most likely tsunami-generating mechanism at Santorini.

    • P. Nomikou
    • T. H. Druitt
    • M. M. Parks
    ResearchOpen Access
    Nature Communications
    Volume: 7, P: 1-10