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SeaSALT aims to redefine the understanding of seafloor spreading by modeling the interactions between magmatic and tectonic events. This research will enhance knowledge of ocean dynamics and improve hazard forecasting for coastal populations and infrastructure.
Seafloor spreading is the process that single-handedly shapes 2/3 of our planet, modulates the dynamics of deep ocean currents, controls the composition of seawater, and supports unique ecosystems that thrive in extreme environments.
Discovered in the 1960s, it is now explained as the slow and steady divergence of 2 tectonic plates accommodated by magma emplacement and faulting at a mid-ocean ridge axis.
In the current paradigm, the texture of the seafloor is primarily determined by the magmatic…
CENTRE NATIONAL DE LA RECHERCHE SCIENTIFIQUE CNRS
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