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Showing 1–2 of 2 results
Advanced filters: Author: Elia d’Acremont Clear advanced filters

  • During the early stages in the formation of divergent margins, the lithosphere experiences large changes in temperature that can determine its strength and influence magma generation. Heat-flow data from the Eastern Gulf of Aden indicate a thermal anomaly that has persisted after continental break-up. This anomaly may have been caused by small-scale convection that occurred during and after rifting.

    • Francis Lucazeau
    • Sylvie Leroy
    • Khalfan Al-Toubi
    Research
    Nature Geoscience
    Volume: 1, P: 854-858

  • The Al-Idrissi Fault System in the Alboran Sea is a major tectonic structure in its initial stage. By using bathymetric and seismic reflection data, the authors unravel a 3D geometry for the AIFS, which corresponds to a crustal-scale boundary and provides a unique model of the inception and growth of a young plate boundary fault system.

    • Eulàlia Gràcia
    • Ingo Grevemeyer
    • César R. Ranero
    ResearchOpen Access
    Nature Communications
    Volume: 10, P: 1-12