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Cannat Mathilde

Fault scarps and tectonic strain in young volcanic seafloor
Beyond Spreading Rate：Controls on the Thermal Regime of Mid-Ocean Ridges
Evolution of enhanced magmatism at the ultraslow spreading Southwest Indian Ridge between 46°E and 53.5°E
Microseismicity and lithosphere thickness at a nearly-amagmatic oceanic detachment fault system
Thermal Regime of Slow and Ultraslow Spreading Ridges Controlled by Melt Supply and Modes of Emplacement
780 thousand years of upper-crustal construction at a melt-rich segment of the ultraslow spreading Southwest Indian Ridge 50°28'E

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