Continental exhumation triggered by partial melting at ultrahigh pressure, Geology, vol.39, issue.12, pp.1171-1174, 2011. ,
DOI : 10.1130/G32316.1
URL : https://hal.archives-ouvertes.fr/insu-00639605
Experimental and theoretical constraints on melt distribution in crustal sources: the effect of crystalline anisotropy on melt interconnectivity, Chemical Geology, vol.124, issue.3-4, pp.161-184, 1995. ,
DOI : 10.1016/0009-2541(95)00052-N
Fabric analysis using the intercept method, Tectonophysics, vol.267, issue.1-4, p.731, 1996. ,
DOI : 10.1016/S0040-1951(96)00091-1
Partially Molten Middle Crust Beneath Southern Tibet: 734 Synthesis of Project INDEPT Results, Science, pp.1684-1688, 1996. ,
Petrogenesis of Migmatites in Maine, p.755, 2001. ,
A petrogenitic grid for pelitic shichts in the system SiO, pp.2-757, 1989. ,
The glass-transition, structural relaxation and shear viscosity of 4b. b) Glass associated to micas White arrows: glass films along muscovite ? quartz 852 boundaries often associated with newly formed peritectic phases (blue) Glass with newly 853 formed peritectic phases is only found close to micas, Black arrows: glass always associated 854 to newly formed peritectic phases along mica cleavage. c) Glass filled crack, p.855, 1996. ,