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Mathieu Rodriguez

Researcher at École Normale Supérieure

Publications -  24
Citations -  409

Mathieu Rodriguez is an academic researcher from École Normale Supérieure. The author has contributed to research in topics: Fracture zone & Transform fault. The author has an hindex of 10, co-authored 22 publications receiving 318 citations. Previous affiliations of Mathieu Rodriguez include Indiana Statewide Testing for Educational Progress-Plus & Centre national de la recherche scientifique.

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Neotectonics of the Owen Fracture Zone (NW Indian Ocean): Structural evolution of an oceanic strike-slip plate boundary

TL;DR: In this paper, the authors studied the structural evolution of the Owen Fracture Zone from Pliocene to present and determined the durability of relay structures and the timing of their evolution along the principal displacement zone from their inception to their extinction.
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Owen Fracture Zone: The Arabia–India plate boundary unveiled

TL;DR: In this article, a high-resolution multibeam echo-sounder was used to search for active faults in the Owen Fracture Zone at the boundary between the Arabia and India plates in the NW Indian Ocean.
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Late Quaternary megaturbidites of the Indus Fan: Origin and stratigraphic significance

TL;DR: In this paper, the authors focus on a Late Quaternary channel-levee system from the Indus Fan captured by the recent opening of the 20°N pull-apart basin, located at 850 km off the present-day Indus Delta, along the OFZ.
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Owen Ridge deep-water submarine landslides: implications for tsunami hazard along the Oman coast

TL;DR: In this article, the authors assess the severity of this potential hazard by performing numerical simulations of tsunami generation and propagation from the biggest landslide (40 km3 in volume) observed along the Owen Ridge.
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Mass wasting processes along the Owen Ridge (Northwest Indian Ocean)

TL;DR: In this paper, the authors present a synthetic map of the different types of mass wasting features observed along the Owen Ridge and further establish a morphometric analysis of submarine landslides, showing that the spatial variation of failure morphology is strongly related to the topography of the basement.