Philippe Matte
University of Montpellier
8 Papers
161 Citations
Philippe Matte is an academic researcher from University of Montpellier. The author has contributed to research in topics: Continental crust & Subduction. The author has an hindex of 7, co-authored 8 publications.
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Papers
A model of palaeozoic obduction and exhumation of high-pressure/low-temperature rocks in the southern urals
TL;DR: In this article, a new evolutionary geodynamic model of Devonian continental subduction and exhumation of high-pressure/low-temperature metamorphic rocks in the southern Urals is proposed based on the results of physical modelling, geological and geophysical data, and on the comparison of this belt with other orogens.
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Première datation UPb des orthogneiss œillés de la zone axiale de la Montagne noire (Sud du Massif central) : nouveaux témoins du magmatisme ordovicien dans la chaı̂ne Varisque
TL;DR: In this paper, Roger et al. date pour la premiere fois par la methode U-Pb sur zircons, les orthogneiss œilles d'affinite calco-alcaline which constituent le cœur du dome gneissique.
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La zone axiale hercynienne de la Montagne Noire n'est pas un “metamorphic core complex” extensif mais un anticlinal post-nappe à cœur anatectique
TL;DR: In this article, a tente d'expliquer lu formation des domes gneissiques de la chaine hercynienne and notamment celui de la Montagne Noire (Sud du Massif Central francais), par un modele purement extensif de type "Basin and Range" is discussed.
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A 3D model of the India-Asia collision at plate scale
TL;DR: A 3D model of the evolution of the India-Asia collision-subduction system from the collision (55 Ma) until now is presented in this paper, where the authors propose some 3D images of this history.
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Les plis hercyniens kilométriques couchés vers l'ouest-sud-ouest dans la région du pic du Midi d'Ossau-col du Somport (zone axiale des Pyrénées occidentales)
TL;DR: The Palaeozoic of the western Pyrenees shows two superposed tectonics easily defined by their different geometry and the major unconformity of the Permian sediments and volcanics on the Devono-Carboniferous series.
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