Author

Sayed Murtadha

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Recent research

  • Climate & Environment

    Mélange diapir origin for Neo-Tethyan ridge-subduction magmatism

    The mélange diapir model invokes physical mixing of partially melted slab components with mantle wedge peridotite, enabling material transfer from the subducted slab to the overlying mantle wedge. However, identifying distinctive igneous rock suites generated through this process...

    Geological Society of America Bulletin2026-08-180 citationsDOI