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Seafloor spreading on Short And Long Time scales

Project description

Cracking the code of the seafloor

Deep beneath the ocean’s surface, a hidden mechanism shapes two-thirds of the Earth – seafloor spreading. This slow-motion drama unfolds at mid-ocean ridges, where it sculpts the planet and feeds strange life in the deep. Yet, scientists still do not know why the seafloor's texture varies so much, or what controls the balance between magma flow and tectonic faulting. The ERC-funded SeaSALT project is diving into this mystery. By reimagining seafloor spreading as a sequence of connected earthquakes, magma intrusions and subtle shifts in stress, researchers will test their ideas through innovative computer models and groundbreaking seafloor observations. SeaSALT could transform how we understand the making of our oceans, and help protect people and infrastructure from volcanic and tectonic hazards.

Objective

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 magmatically-accommodated fraction (M) of plate separation at the ridge axis. However, we do not know what sets the M fraction in the first place, and why it is subject to spatiotemporal fluctuations that can cause drastic shifts in seafloor spreading regimes. SeaSALT tackles this issue by rethinking seafloor spreading as a succession of discrete magmatic and tectonic events which, by inhibiting or triggering one another, self-consistently distribute magmatic and tectonic strain. To test this hypothesis, we will design brand-new simulations of seismo-volcanic cycles in which dike intrusions, earthquakes, or aseismic slip transients may occur in response to far-field extension and pressurization of a shallow magma reservoir. Each component of the model will be constrained by groundbreaking observations of seafloor spreading events and inter-event stress build-up at 3 target sites. This includes the most ambitious seafloor seismo-geodesy experiment to date across a ridge axis, and the development of a novel hydrothermal geodesy method that constrains sub-seafloor stress changes via the perturbations they impart on black smoker temperatures. The success of our new framework will be indexed on its ability to spontaneously generate the types of events documented at each site, while accounting for the M fraction and its multiscale variability, as recorded in high-resolution bathymetry. It will also help forecast hazards to rift populations and key submarine infrastructure.

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HORIZON-ERC - HORIZON ERC Grants

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Call for proposal

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(opens in new window) ERC-2024-COG

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Host institution

CENTRE NATIONAL DE LA RECHERCHE SCIENTIFIQUE CNRS
Net EU contribution

Net EU financial contribution. The sum of money that the participant receives, deducted by the EU contribution to its linked third party. It considers the distribution of the EU financial contribution between direct beneficiaries of the project and other types of participants, like third-party participants.

€ 1 999 804,00
Total cost

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€ 1 999 804,00

Beneficiaries (1)

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