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charged GAGs which, when combined with collagen, produce an osmotic effect. The fluid-structure interaction will be modelled as a homogenised continuous medium within the framework of poromechanics, while
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structures and image the circulation of fluids in the Ecuadorian subduction zone in order to determine their role in seismic and aseismic slip. Where to apply Website https://emploi.cnrs.fr/Candidat/Offre
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