The thermal structure of subduction zones constrained by seismic imaging: Implications for slab dehydration and wedge flow, Earth and Planetary Science Letters, vol.241, issue.3-4, pp.241-387, 2006. ,
DOI : 10.1016/j.epsl.2005.11.055
Omphacite fabric variation in the Cabo Ortegal eclogite (NW Spain): relationships with strain symmetry during high-pressure deformation, Journal of Structural Geology, vol.19, issue.5, pp.621-637, 1997. ,
DOI : 10.1016/S0191-8141(97)00001-1
Orientation imaging: The emergence of a new microscopy, Metallurgical Transactions A, vol.23, issue.4, pp.819-831, 1993. ,
DOI : 10.1016/0956-7151(92)90413-9
70-80???km) continuous slice of oceanic lithosphere detached from a subduction zone?, Terra Nova, vol.112, issue.3, pp.171-180, 2009. ,
DOI : 10.1111/j.1365-3121.2009.00870.x
URL : https://hal.archives-ouvertes.fr/hal-00401406
Subduction interface processes recorded by eclogite-facies shear zones (Monviso, W. Alps), Lithos, vol.127, issue.1-2, pp.222-238, 2011. ,
DOI : 10.1016/j.lithos.2011.09.004
URL : https://hal.archives-ouvertes.fr/insu-00624611
Eclogite breccias in a subducted ophiolite: A record of intermediate-depth earthquakes?, Geology, vol.40, issue.8, pp.40-707, 2012. ,
DOI : 10.1130/G32925.1
URL : https://hal.archives-ouvertes.fr/insu-00723238
Probing the transition between seismically coupled and decoupled segments along an ancient subduction interface, Geochemistry, Geophysics, Geosystems, vol.112, issue.2, pp.16-1905, 2015. ,
DOI : 10.1029/2006JB004441
URL : https://hal.archives-ouvertes.fr/hal-01243526
Fluid pathways and high pressure metasomatism in a subducted continental slice (Mt. Emilius klippe, W. Alps), Journal of Metamorphic Geology, 2017. ,
URL : https://hal.archives-ouvertes.fr/insu-01489148
A revision of the garnet-clinopyroxene Fe 2+ -Mg exchange Planetary Science Letters, pp.75-86, 1994. ,
Petrofabric studies of eclogite, spinel-Websterite, and spinel-lherzolite Xenoliths from kimberlite-bearing breccia pipes in southeastern Utah and northeastern Arizona, Journal of Geophysical Research, vol.3, issue.9, pp.4350-4365, 1972. ,
DOI : 10.1029/JB077i023p04350
algorithm, Journal of Applied Crystallography, vol.41, issue.6, pp.1024-1037, 2008. ,
DOI : 10.1107/S0021889808030112
Earthquakes in the ductile regime?, Pure and Applied Geophysics, pp.309-336, 1986. ,
DOI : 10.1007/BF00875730
Disequilibrium metamorphism of stressed lithosphere, Earth-Science Reviews, vol.154, pp.1-13, 2016. ,
DOI : 10.1016/j.earscirev.2015.12.002
Partial eclogitisation of gabbroic rocks in a late Precambrian subduction zone (Zambia): prograde metamorphism triggered by fluid infiltration, Contributions to Mineralogy and Petrology, vol.146, issue.2, pp.174-191, 2003. ,
DOI : 10.1007/s00410-003-0492-8
Interrelations between intermediate-depth earthquakes and fluid flow within subducting oceanic plates: Constraints from eclogite facies pseudotachylytes, Geology, vol.34, issue.7, pp.557-560, 2006. ,
DOI : 10.1130/G22411.1
URL : http://www.gsajournals.org/pdfserv/?doi=10.1130%2FG22411A.1
High-pressure metamorphism and deep-crustal seismicity: evidence from contemporaneous formation of pseudotachylytes and eclogite facies coronas, Tectonophysics, vol.372, issue.1-2, pp.59-83, 2003. ,
DOI : 10.1016/S0040-1951(03)00232-4
Calculating anisotropic physical properties from texture data using the MTEX open-source package, Geological Society, London, Special Publications, vol.360, issue.1, pp.175-192, 2011. ,
DOI : 10.1144/SP360.10
URL : https://hal.archives-ouvertes.fr/hal-00688833
Die Nomenklatur von Pyroxenen, Mineralogy and Petrology, vol.62, issue.1, pp.55-76, 1988. ,
DOI : 10.1007/BF01226262
Crystalline Plasticity and Solid State Flow in Metamorphic Rocks, 1976. ,
The generation of ductile and brittle shear bands in a low-angle mylonite zone, Journal of Structural Geology, vol.6, issue.3, pp.273-281, 1984. ,
DOI : 10.1016/0191-8141(84)90051-8
Evoluzione strutturale del M. Emilius (Austroalpino, Alpi occidentali), Rend. Soc. Geol. It, vol.14, pp.97-100, 1991. ,
Progressive eclogitization under fluid-present conditions of pre-Alpine mafic granulites in the Austroalpine Mt Emilius Klippe (Italian Western Alps), Journal of Structural Geology, vol.18, issue.5, pp.549-561, 1996. ,
DOI : 10.1016/S0191-8141(96)80023-X
Ductile-brittle transition in pre-Alpine amphibolite facies mylonites during evolution from water-present to water-deficient conditions (Mont Mary nappe, Italian Western Alps), Journal of Metamorphic Geology, vol.15, issue.6, pp.777-791, 1997. ,
DOI : 10.1111/j.1525-1314.1997.00055.x
Control of the geometry of precursor brittle structures on the type of ductile shear zone in the Adamello tonalites, Southern Alps (Italy), Journal of Structural Geology, vol.27, issue.4, pp.627-644, 2005. ,
DOI : 10.1016/j.jsg.2004.11.008
Nucleation and initial growth of a shear zone network within compositionally and structurally heterogeneous granitoids under amphibolite facies conditions, Journal of Structural Geology, vol.29, issue.11, pp.29-1757, 2007. ,
DOI : 10.1016/j.jsg.2007.06.002
Trace-element-rich brines in eclogitic veins: implications for fluid composition and transport during subduction, Contributions to Mineralogy and Petrology, vol.64, issue.3, pp.417-430, 1991. ,
DOI : 10.1007/BF00321985
Deformation processes in eclogitic rocks: evidence for the rheological delamination of the oceanic crust in deeper levels of subduction deformed omphacites, Tectonophysics, vol.78, pp.403-418, 1992. ,
An eclogite-bearing continental tectonic slice in the Zermatt???Saas high-pressure ophiolites at Trockener Steg (Zermatt, Swiss Western Alps), Lithos, vol.232, 2015. ,
DOI : 10.1016/j.lithos.2015.07.010
Abbreviations for names of rock-forming minerals, American Mineralogist, vol.95, issue.1, 2010. ,
DOI : 10.2138/am.2010.3371
Metamorphic record of catastrophic pressure drops in subduction zones, Nature Geoscience, vol.116, issue.1, pp.46-50, 2017. ,
DOI : 10.1038/ngeo2852
URL : https://hal.archives-ouvertes.fr/insu-01409600
Top right inlay in d): X-ray chemical map presenting the Ca content variations of a garnet assemblage. (Mineral abbreviations are the same than in Fig ,