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Showing 1–10 of 10 results
Advanced filters: Author: Jonas Preine Clear advanced filters
  • Regional volcanism in the Terror Rift is influenced by deep-seated tectonic and magmatic processes as well as surficial factors, such as the advancement and retreat cyclicity of ice sheets, as evidenced by mapping and sampling of seafloor volcanism in the southwestern Ross Sea.

    • Masako Tominaga
    • Kurt Panter
    • Thea Rae
    ResearchOpen Access
    Communications Earth & Environment
    Volume: 6, P: 1-7
  • Evidence for a past large explosive eruption within the Santorini caldera suggests that early stages of silicic caldera cycles can be more hazardous than previously assumed, according to analyses of intra-caldera deposits from the Kameni Volcano.

    • Jonas Preine
    • Jens Karstens
    • Dimitrios Papanikolaou
    ResearchOpen Access
    Nature Geoscience
    Volume: 17, P: 323-331
  • The authors use seismic and sedimentology data to estimate the volume of the Minoan eruption. The results show that the Plinian phase contributed most to the distal tephra fall, and that the pyroclastic flow volume is significantly smaller than previously assumed.

    • Jens Karstens
    • Jonas Preine
    • Christian Berndt
    ResearchOpen Access
    Nature Communications
    Volume: 14, P: 1-10
  • Seismological and geodetic data are used together with a machine learning earthquake catalogue to reconstruct magma migration before and during the 2025 volcano–tectonic crisis at Santorini volcano, indicating a coupling between Santorini and Kolumbo.

    • Marius P. Isken
    • Jens Karstens
    • Christian Berndt
    ResearchOpen Access
    Nature
    Volume: 645, P: 939-945
  • Effusive volcanism dominates at water depths of 300 m or greater while phreatomagmatic Surtseyan eruptions become prevalent at shallower depths, according to analyses of high-resolution seismic reflection profiles, multibeam bathymetry, and seafloor imagery.

    • Jonas Preine
    • Christian Hübscher
    • Nico Augustin
    ResearchOpen Access
    Communications Earth & Environment
    Volume: 7, P: 1-16
  • The Zanclean megaflood poured water from the western to the eastern Mediterranean basin through a shallow marine corridor in south-eastern Sicily, ending the isolation of the Mediterranean Sea from the global oceans about 5.3 million years ago, according to onshore-offshore geological data from southern Sicily and numerical modelling.

    • Aaron Micallef
    • Giovanni Barreca
    • Antonio Caruso
    ResearchOpen Access
    Communications Earth & Environment
    Volume: 5, P: 1-11