Agard, P., P. Monié, et al. (2002). “Exhumation of the Schistes Lustrés complex: in situ laser probe Ar/Ar constraints and implications for the Western Alps.” Journal of Metamorphic Geology 20: 599-618

Allemand, P. and J. M. Lardeaux (1997). “Strain partioning and metamorphism in a deformable orogenic wedge: application to the Alpine belt.” Tectonophysics 280: 157-169.

Amato, J. F., C. M. Johnson, et al. (1999). “Rapid exhumation of the Zermatt Saas ophiolite deduced from high precison Sm-Nd and Rb-Sr geochronology.” Earth and Planet Science Letters 171: 425-438.

Arnaud, N. O. and S. P. Kelley (1995). “Evidence for excess argon during high pressure metamorphism in the Dora Maira Massif (western Alps, Italy), using an ultra-violet laser ablation microprobe 40Ar-39Ar technique.” xxxxxx121: 1-11.

Auzende, A. L., Devouard, B., Guillot, S., Daniel, I.Baronnet, A., Lardeaux, J.M. (2002). “Serpentinites from Central Cuba: petrology, and HRTEM study.” European Journal of Mineralogy 14: 905-914.

Auzende, A. L., S. Guillot, et al. (2005). “Behavior of serpentinites in convergent context: microstructural evidences.” European Journal of Mineralogy in press.

Ballèvre, M., Y. Lagabrielle, et al. (1990). “Tertiary ductile normal faulting as a consequence of lithospheric stacking in the Western Alps.” Société Géologique de France, mémoires 156: 227-236.

Billen, M. I. and M. Gurnis (2003). “Comparison of dynamic flow models for the Central Aleutian and Tonga-Kermadec subduction zones.” Geochemistry Geophysics Geosystems 1035 doi:10 1029/2001GC000295.

Blake, C. and A. S. Jayko (1990). “Uplift of high pressure rocks in the Western Alps: evidence of structural attenuation along low angle normal faults.” Mémoire de la Socièté Géologique de france 156: 228-237.

Blake, C., D. G. Moore, et al. (1995). “The role of the serpentinite melange in the unroofing of the UHP rocks: an example from the western Alps in Italy.” from Coleman R.G. and Wang X. (eds). Ultrahigh pressure metamorphism. Cambridge University Press: 182-205.

Bostock, M. G., and. Hydman, R.D., et al. (2002). “An inverted contienntal Moho and serpentinization of the forearc mantle.” Nature 417: 536-538.

Castelli, D., C. Rostagno, et al. (2002). “Jd-QTZ-bearing metaplagiogranite from the Monviso meta-ophiolite (Western Alps).” Ofioliti 27: 81-90.

Chemenda, A. I., M. Mattauer, et al. (1996). “Continental subduction and a mechanism for exhumation of high-pressure metamorphic rocks: new modeling and field data from Oman.” Earth Planetary Science Letters 143: 173-185.

Chopin, C. and H. B. Schertl (1999). “The UHP unit in the Dora Maira massif, western Alps.” International Geology Reviews 41: 765-780.

Cliff, R. A., Barnicoat, A.C. and Inger,S. (1998). “Early Tertiary eclogite facies metamorphism in the Monviso Ophiolite.” Journal metamorphic geology 16: 447-455.

Cloos, M. (1982). “Flow melanges : numerical modelling and geological constraints on their origin in the Franciscan subduction complex.” Geological Society of America Bulletin 93: 330-345.

Cloos, M. and R. L. Shreve (1988). “Subduction channel model of prism accretion, melange formation, sediment subduction, and subducting erosion at convergent plate margins: 1. Background and description, in subduction zone Part 1.” Pageophysics 128: 501-545.

de Sigoyer, J., S. Guillot, et al. (2004). “Exhumation Processes of the high-pressure low-temperature Tso Morari dome in a convergent context (eastern-Ladakh, NW-Himalaya).” Tectonics Vol. 23, No. 3, TC3003 - 10.1029/2002TC001492.

Deville, E. (1986). “La klippe de la pointe du grand Vallon (Vanoise, Alpes Occidentales): un lambeau de métasédiments à foraminifères du Maastrichien Supérieur couronnant les nappes de Schistes Lustrés.” Compte-rendus de l'Académie des Sciences 303: 1211-1226.

Deville, E., S. Fudral, et al. (1992). “From oceanic closure to continental collision: a synthesis of the Schistes Lustrés metamorphic complex of the Western Alps.” Geological Society of America 104: 127-139.

Duchêne, S., J. Blichert-Toft, et al. (1997a). “The Lu-Hf dating of garnets and the ages of the Alpine high-pressure metamorphism.” Nature 387: 586-589.

Duchene, S., J. M. Lardeaux, et al. (1997). “Exhumation of eclogites: Insights from retrograde depth-time path analysis.” Tectonophysics 280: 125-140.

Duchêne, S., J. M. Lardeaux, et al. (1997). “Exhumation of eclogites: insights from depth-time path analysis.” Tectonophysics 280.

Eide, E. A. and J. G. Liou (2000). “High Pressure blueschists and eclogites in Hong'an: a framework for adressing the evolution of high and ultrahigh-pressure rocks in central China.” Lithos 52: 1-22.

Ernst, W. G. (2001). “Subduction, ultrahigh-pressure metamorphism, and regurgitation of buoyant crustal slices - implications for arcs and continental growth.” Physical of Earth Planetary Interior 127: 253-275.

Escher, A., J. Hunziker, et al. (1997). “Geologic framework and structural evolution of the Western Swiss-Italian Alps.” In Pfinner O.A., Lehner, P., Heitzmann, P., Mueller, S., Steck (Eds). Deep structure of the Swiss Alps. Results of NRP 20. Birkhäusser Verlag, basel.: 205-211

Facenna, C., T. W. Becker, et al. (2001). “History of subdcution and and back arc extension in the central Mediterranean.” Geophysical Journal Interiors 145: 809-820.

Garcia-Casco, A. G., R. L. Torres-Roldan, et al. (2002). “Oscillatory zoning in eclogitic garnet and amphibole northern serpentinite melange, Cuba: a record of tectonic instability.” Journal of Metamorphic Geology 20: 581-598.

Gebauer, D., H. B. Schertl, et al. (1997). “35 Ma old ultra-high pressure metamorphism and evidence for very rapid exhumation in the Dora Maira massif, Western Alps.” Lithos 41: 5-24.

Gerya, T. V. and B. Stöckert (2002). “Exhumation rates of high pressure metamorphic minerals in subduction channels: the effect of rheology.” Geophysical Research Letters 29: 102-1 TO 102-4.

Gerya, T. V., B. Stöckert, et al. (2002). “Exhumation rates of high pressure metamorphic minerals in subduction channels: a numerical simulations.” Tectonics 21: 1056, doi:10.1029/2002TC001406.

Goncalvez, P., S. Guillot, et al. (2000). “Thrusting and sinistral wrenching in a pre-Eocene carribean accretionary wedge (Samana pensinsula -Dominican Republic).” Geodinamica Acta 13: 119-132.

Guillot, S., E. Garzanti, et al. (2003). “Reconstructing the total shortening history of the NW Himalaya.” Geochem. Geophys. Geosyst., 4(1), XXXX, doi:10.1029/2002GC000484.

Guillot, S., K. Hattori, et al. (2000). “Mantle wedge serpentinization and exhumation of eclogites: insights from eastern Ladakh, northwest Himalaya.” Geology 28: 199-202.

Guillot, S., K. Hattori, et al. (2001). “Evidence of hydration of the mantle wedge and its role in the exhumation of eclogites.” Earth and Planetary Sciences Letters 193: 115-127.

Hacker, B. R., L. Ratschbacher, et al. (2000). “Exhumation of ultrahigh-pressure continental crust in east central China; Late Triassic-Early Jurassic tectonic unroofing.” Journal of Geophysical Research, B, Solid Earth and Planets 105(6): 13,339-13,364.

Hermann, J., O. Müntener, et al. (2000). “The importance of serpentinite mylonites for subduction and exhumation of oceanic crust.” Tectonophysics 327: 225-238.

Hirth, G. and D. Kohlstedt (2003). “Rheology of the upper mantle and the mantle wedge: a view from the experimentalists.” Geophysical Monograph Series,Inside the Subduction Factory 138: 83-105.

Labrousse, L., L. Jolivet, et al. (2002). “Crustal scale boudinage and migmatization of gneiss during their exhumation in the UHP province of Western Norway.” Terra Nova 14: 263-270.

Lagabrielle, Y. and M. Cannat (1990). “Alpine Jurassic ophiolites resemble the modern central Atlantic basement.” Geology 18: 319-322.

Lagabrielle, Y. and a. others (1984). “Les témoins d'une tectonique intraocéanique dans le domaine téthysien: analyse des rapports entre les ophiolites et leur couverture métasédimentaire dans la zone piédmontaise des Alpes Franco-Italiennes.” Ofioliti 9: 67-88.

Le Fort, P., S. Guillot, et al. (1997). “HP metamorphic belt along the Indus suture zone of NW Himalaya : new discoveries and significance.” Compte Rendus de l'Académie des Sciences, Paris 325: 773-778.

Lemoine, M., P. Tricart, et al. (1987). “Ultramafic and gabbroic ocean floor of the Ligurian Tethys (Alps, Corsica, Apennines): in search of a genetic model.” Geology 15: 622-625.

Li, X. P., M. Rahn, et al. (2004). “Serpentinites of the Zermatt-Saas ophiolite complex and their texture evolution.” Journal of Metamorphic Geology 22: 159-177.

Lombardo, B., R. Nervo, et al. (1978). “Osservazioni preliminari sulle ofioliti metamorfiche del monviso (Alpi occidentali).” Rendiconti Societa Italiana di Mineralogia e Petrologia 34: 253-305.

Lombardo, B., D. Rubatto, et al. (2002). “Ion microprobe U-Pb dating of zircon from a Monviso metaplagiogranite: implications for the evolution of the Piedmont-Liguri Tethys in the western Alps.” Ofioliti 27: 109-117.

Meffan-Main, F., R. A. Cliff, et al. (2004). “A Tertiary age for Alpine metamorphism in the Gran Paradiso massif, western Alps: a Rb-Sr microsampling study.” Journal of Metamorphic Geology 22: 267-281.

Messiga, B., J.-R. Kienast, et al. (1999). “Cr-rich magnesio-chloritoid eclogites from the Monviso ophiolites (Western Alps, Italy).” Journal of Metamorphic Geology 17: 287-299.

Mevel, C. (2003). “Serpentinization of abyssal peridotites at mid-ocean ridges.” Comptes Rendus Géoscience 335: 825-852.

Mevel, C., R. Caby, et al. (1978). “Lower amphibolite facies conditions in the oceanic cruts: example of amphibolitized falser-gabbro and amphibolites from an alpine ophiolitic massif (Chenaillet massif, Hautes Alpes, France).” Earth and Planet Science Letters 39: 98-108.

Monie, P. and C. Chopin (1991). “Ar dating in coesite-bearing and associated units of the Dora Maira massif, Western Alps.” Eur.J.Mineral. 3: 239-262.

Monié, P. and P. Philippot (1989). “Mise en évidence de l'âge Eocène moyen du métamorphisme de haute pression dans la nappe ophiolitique du Monviso (Alpes Occidentales) par la méthode Ar-Ar.” Compte-rendus de l'Académie des Sciences 309: 245-251.

Nadeau, S., P. Philippot, et al. (1993). “Fluid inclusion and mineral isotopic composition (H-C-O) in eclogitic rocks as tracers of local fluid migration during high pressure metamorphism.” Earth and Planet Science Letters 114: 431-448.

Paul, A., M. Cattaneo, et al. (2001). “A three-dimensional crustal velocity model of the southwesternAlps from the local earthquake tomography.” Journal Geophysical Research 106: 19367-19389.

Philippot, P., P. Agrinier, et al. (1998). “Chlorine cycling during subduction of altered crust.” Earth and Planetary Science Letters 161: 33-44.

Piccardo, G. B., E. Rampone, et al. (2001). “Evolution of the Ligurian Tethys: inference from petrology and geochemistry of the Ligurian Ophiolites.” Per. Mineralogy 70: 147-192.

Platt, J. P. (1986). “Dynamic of orogenic wedges and the uplift of high-pressure metamorphic rocks.” Bulletin of Geological Society of America 97: 1037-1053.

Platt, J. P. (1993). “Exhumation of high-pressure metamorphic rocks : a review of concepts and processes.” Terra Nova 5: 119-133.

Polino, R., G. V. Dal Piaz, et al. (1990). “Tectonic erosion at the Adria margin and accretionary processes for the Cretaceous orogeny of the Alps.” Mémoire de la Socièté Géologique de France 156: 345-367.

Rosenbaum, G. and G. S. Lister (2005). “The Western Alps from the Jurassic to Oligocene: spatio-temporal constraints and evolutionary reconstructions.” Earth Science Reviews 69: 281-306.

Rubatto, D. and J. Hermann (2001). “Exhumation as fast as subduction ?” Geology 29: 3-6.

Rubatto, D. and J. Hermann (2003). “Zircon formation during fluid circulation in eclogites (Monviso Western Alps): implications for Zr and Hf budget in subduction zones.” Geochimica and Cosmochimica Acta 67: 2173-2187.

Scambelluri, M., O. Muntener, et al. (1995). “Subduction of water into the mantle: history of an alpine peridotite.” Geology 23: 459-462.

Schettino, A. and C. Scotese (2002). “Global kinematic constraints to the tectonic history of the mediterranean region and surrounding areas during the Jurassic and Cretaceous.” Journal of Virtual Explorer 8: 145-160.

Schwartz, S. (2001). La zone piémontaise des Alpes occidentales: un paléo-complexe de subduction; arguments métamorphiques, géochronologiques et structuraux. Documents du BRGM, vol. 302, 313 pp.

Schwartz, S., P. Allemand, et al. (2001). “Numerical model of the effect of serpentinites on the exhumation of eclogitic rocks : insights from the Monviso ophiolitic massif (Western Alps).” Tectonophysics 42: 193-206.

Schwartz, S., J. M. Lardeaux, et al. (2000). “Diversité du métamorphisme éclogitique dans le massif ophiolitique du Monviso 'Alpes Occidentales, Italie).” Geodinamica Acta 13: 169-188.

Seno, T. and T. Yamasaki (2003). “Low frequency tremors, intraslab and interplate earthquakes in southwest Japan, from a viewpoint of slab dehydration.” Geophysical Research Letters 30: 22 2171- doi 10.1029/2003GLO18349.

Stöckert, B. and T. V. Gerya (2005). “Pre-collisional HP metamorphism and nappe tectonics at active continental margins: a numerical simulation.” Terra Nova doi10.1111/j.1365-3112.2004.00589.

Stöckert, B., M. Wachmann, et al. (1999). Tectonophysics 303: 299-319.

Tricart, P., S. Schwartz, et al. (2004). “Evidence for synextensional tilting and doming during during final exhumation from analysismultistage faults (Queyras, Schsites Lustrés, Western Alps).” Journal of Structural Geology 26: 1633-1645.

Vidal, O., T. Parra, et al. (2001). A thermodynamic model for Fe-Mg aluminous chlorite using data from phase equilibrium experiments and natural pelitic assemblages in the100-600°C, 1-25 kbar P-T range. American journal of Science, 301, 557-592.