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  • Results from a high-resolution ocean-bottom seismometer experiment at the ultraslow-spreading Gakkel Ridge show unexpected highly variable crustal thickness and a relatively large average value, which can be explained by an active mantle upwelling model.

    • Tao Zhang
    • Jiabiao Li
    • Jason P. Morgan
    ResearchOpen Access
    Nature
    Volume: 633, P: 109-113