M
Martine Simoes
Researcher at Institut de Physique du Globe de Paris
Publications - 47
Citations - 1433
Martine Simoes is an academic researcher from Institut de Physique du Globe de Paris. The author has contributed to research in topics: Subduction & Tectonics. The author has an hindex of 17, co-authored 38 publications receiving 1180 citations. Previous affiliations of Martine Simoes include California Institute of Technology & University of Paris.
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Late Cenozoic metamorphic evolution and exhumation of Taiwan
Olivier Beyssac,Olivier Beyssac,Martine Simoes,Martine Simoes,Martine Simoes,Jean Philippe Avouac,Kenneth A. Farley,Yue-Gau Chen,Yu-Chang Chan,Bruno Goffé +9 more
TL;DR: In this paper, the authors apply this technique in addition to (U-Th)/He thermochronology on detrital zircons to assess peak metamorphic temperatures (T) and the late exhumational history respectively, along different transects in central and southern Taiwan.
Journal ArticleDOI
Rupture process of the Mw = 7.9 2015 Gorkha earthquake (Nepal): Insights into Himalayan megathrust segmentation
Raphaël Grandin,Martin Vallée,Claudio Satriano,Robin Lacassin,Yann Klinger,Martine Simoes,Laurent Bollinger +6 more
TL;DR: In this article, the authors investigated the rupture process of the 25 April 2015 Gorkha earthquake using a kinematic joint inversion of teleseismic waves, strong motion data, high-rate GPS, static GPS, and synthetic aperture radar (SAR) data.
Rupture process of the Mw7.9 2015 Gorkha earthquake (Nepal): insights into Himalayan megathrust segmentation
Raphaël Grandin,Martin Vallée,Claudio Satriano,Robin Lacassin,Yann Klinger,Martine Simoes,Laurent Bollinger +6 more
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Mountain building in Taiwan: A thermokinematic model
Martine Simoes,Martine Simoes,Martine Simoes,Jean Philippe Avouac,Olivier Beyssac,Bruno Goffé,Kenneth A. Farley,Yue-Gau Chen +7 more
TL;DR: In this paper, a new thermokinematic model of the Taiwan mountain belt reconciling existing kinematic, thermometric and thermochronological constraints is proposed, which shows that a significant contribution of underplating to the growth of the orogenic wedge is made by the most frontal faults of the foothills.
Journal ArticleDOI
The Sumatra subduction zone: A case for a locked fault zone extending into the mantle
TL;DR: In the case of the Sumatra subduction zone where the downdip end of the locked fault zone (LFZ) can be well constrained from the pattern and rate of uplift deduced from coral growth and from GPS measurements of horizontal deformation, this paper showed that the LFZ most probably extends into the mantle, implying that either the mantle is not serpentinized, or the presence of serpentine does not necessarily imply stable sliding.