La modélisation expérimentale tridimensionnelle thermomécanique de la subduction continentale et l'exhumation des roches de ultra haute pression/basse température

La modélisation expérimentale tridimensionnelle thermomécanique de la subduction continentale et l'exhumation des roches de ultra haute pression/basse température

La distribution spatiale des massifs UHP/BT montre que leur exhumation est un phénomène 3D qui a lieu uni-quement dans des zones particulières des chaînes de montagnes caractérisées par une complexité structurale et/ou géométrique. Dans les expériences de modélisation thermomécanique 2D de la subduc...

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Bibliographic Details
Main Author:	Boutelier, David
Language:	FRE
Published:	Université de Nice Sophia-Antipolis 2004
Subjects:	[SDU:STU:AG] Sciences of the Universe/Earth Sciences/Applied geology Modélisation expérimentale thermo mécanique de la lithosphère subduction continentale exhumation de roches de ultra haut pression orogenèse collision arc-continent collision continent-continent coesite éclogite
Online Access:	http://tel.archives-ouvertes.fr/tel-00005197 http://tel.archives-ouvertes.fr/docs/00/04/64/29/PDF/tel-00005197.pdf

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