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136La transition diagenèse métamorphisme (M. Dubois et F. Bourdelle)

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Bourdelle F., Benzerara K., Beyssac O., Cosmidis J., Neuville D.R., Brown G.E. Jr, et Paineau E. (2013a). – Quantification of the ferric/ferrous iron ratio in silicates by scanning transmission X-ray microscopy at the Fe L2,3 edges. Contributions to Mineralogy and Petrology, 166, p. 423-434.

Bourdelle F., Parra T., Chopin C. et Beyssac O. (2013b). – A new chlorite geothermometer for diagenetic to low-grade metamorphic conditions. Contributionns to Mineralogy and Petrology, 165, p. 723–735.

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Fusion partielle, extraction des liquides et différenciation de la croûte continentale : l’exemple du Massif central français (V. Gardien)

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Sawyer E.W. (2001). – Melt segregation in the continental crust: distribution and movement of melt in anatectic rocks. Journal of Metamorphic Geology, 19 (3), p. 291-309.

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Thompson A.B., Connolly J.A.D. (1995). – Melting of the continental crust: some thermal and petrological constraints on anatexis in continental collision zones and other tectonic settings. Journal Geophysical. Research, 100, p. 15565-15579.

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Vanderhaeghe O. (2009). – Migmatites, granites and orogény: flow model of partially-molten rocks and magmas associated with melt/solid segregation in orogenic belts. Tectonophysics, 477, p. 119-134.

Vielzeuf D., Holloway J.-R. (1988). – Experimental determination of the fluid-absent melting relations in the politic system. Consequences for crustal differenciation. Contribution to Mineralogy and Petrology, 98, p. 257-276.

Vigneresse J.-L., Barbey P., Cuney M. (1996). – Rheological transitions during partial melting and crystallization with application to felsic magma segregation and transfer. Journal of Petrology, 37, p. 1579-1600.

 

Le métamorphisme de (ultra) haute pression : deux siècles de débats (G. Godard)

Les références citées sont disponibles in :

Godard G. (2001). – Eclogites and their geodynamic interpretation: a history. Journal of Geodynamics, 32, p. 165-203.

Godard G., Frezzotti M.-L., Palmeri R., Smith D.C. (2011). – Origin of high-pressure disordered metastable phases (lonsdaleite and incipiently amorphized quartz) in metamorphic rocks: geodynamic shock or crystal-scale overpressure? In: Dobrzhinetskaya, L. Cuthbert, S. Faryad, W. (Eds.), Ultrahigh Pressure Metamorphism: 25 years after discovery of coesite and diamond. Elsevier, Amsterdam, p. 125-148.

 

Métamorphismes extrêmes et refroidissement de la Terre (C. Nicollet)

La bibliographie proposée pour cet article est minimale : les références indiquées ne sont que des exemples dans la nombreuse bibliographie sur le sujet.

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Clark C., Fitzsimons I.C.W., Healy D. and Harley S.L. (2011). – How does the continental crust get really hot? Elements, 7, p. 235-240.

Cross C.B., Diener J.F.A. and Fagereng A. (2015). – Metamorphic imprint of accretion and ridge subduction in the Pan-African Damara Belt, Namibia. J. metamorphic Geol., 33, p. 633-648.

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Vielzeuf D., Holloway J.R. (1988). – Experimental determination of the fluid-absent
melting relations in the pelitic system: consequences for crustal differentiation. Contributions to Mineralogy and Petrology, 98, p. 257-276.

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Les apports de l’expérimentation à la modélisation des processus métamorphiques (T. Hammouda)

Akaogi M., Yusa H., Shiraishi K., Suzuki T. (1995). – Thermodynamic properties of a-quartz, coesite, and stishovite and equilibrium phase relations at high pressures and high temperatures. J. Geophys. Res. 100, p. 22,337-22,347.

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Holland T.J.B. (1980). – The reaction albite = jadeite + quartz determined experimentally in the range 600-1200°C. Amer. Mineral., 65, p. 129-134.

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Le Breton N., Thompson A.B. (1988). – Fluid-absent (dehydration) melting of biotite in metapelite in the early stages of crustal anatexis. Contrib. Mineral. Petrol., 99, p. 226-237.

Moore R.O, Gurney J.J. (1985). – Pyroxene solid solution in garnets included in diamond. Nature, 318, p. 553-555.

Ringwood et Major (1967). – The pyroxene-garnet transformation in the Earth’s mantle. Earth Planet. Sci. Lett., 2, p. 255-263.

Robertson E.C., Birch F., MacDonald J.F. (1957). – Experimental determination of jadeite stability relations to 25,000 bars. Amer. J. Sci., 255, p. 115-137.

Sautter V., Haggerty S.E. and Field F. (1991). – Ultradeep (> 300 kilometers) ultramafic xenoliths: Petrological evidence from the transition zone. Science, 168, p. 832-833.

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Vielzeuf D., Holloway J.R. (1988). – Experimental determination of the fluid-absent melting relations in the pelitic system. Contrib. Mineral. Petrol., 98, p. 257-276.

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Yoder H.S. Jr (1980). – Experimental mineralogy: achievements and prospects. Bull. Mineral., 103, p. 5-26.

Yoder H.S. Jr (1950). – The jadeite problem (Part I and II). Amer. J. Sci., 248, p. 225-248 ; 312-334.

Pour aller plus loin

Il existe plusieurs ouvrages en anglais qui présentent les techniques expérimentales appliquées aux problèmes des sciences de la Terre, dont ceux de Ulmer et Barnes (1987) et de Holloway et Wood (1988). En langue française, le Réseau Technologique des Hautes Pression du CNRS (http://www.reseauhp.org/) a édité des ouvrages qui, sans être restreints aux sciences de la Terre, présentent l’ensemble des techniques de hautes pressions et leurs applications. On peut aussi citer, également en langue française, l’étude de G. Gohau (1996) sur l’historique des études expérimentales appliquées aux problèmes géologiques.

Gohau G. (1996). – Expériences anciennes sur la formation des roches cristallines du dernier quart du dix-huitième siècle aux années 1850. Travaux du Comité français d'Histoire de la Géologie, COFRHIGEO, 3ème série, T.10, p.101-103. <hal-00933424>.

Holloway J.R., Wood B.J. (1988). – Simulating the Earth. Experimental Geochemistry. Unwin Hyman, London, UK, 205 p.

Ulmer G.C., Barnes H.L. (1987). – Hydrothermal Experimental Techniques. John Wiley and Sons, New-York, 538 p.

 

À la recherche de l’équilibre perdu (B. Dubacq)

Agard P., Augier R. and Monié P. (2011). – Shear band formation and strain localization on a regional scale: Evidence from anisotropic rocks below a major detachment (Betic Cordilleras, Spain). Journal of Structural Geology, 33, p. 114-131. doi :10.1016/j.jsg.2010.11.011.

Berman R.G. (1991). – Thermobarometry using multi-equilibrium calculations ; a new technique, with petrological applications. The Canadian Mineralogist, 29, p. 833-855.

Bickle M.J. and McKenzie D. (1987). – The transport of heat and matter by fluids during metamorphism. Contributions to Mineralogy and Petrology, 95, p. 384-392. doi : 10.1007/BF00371852.

Bourdelle F., Benzerara K., Beyssac O., Cosmidis J., Neuville D., Brown Gordon E. J. and Paineau E. (2013). – Quantification of the ferric/ferrous iron ratio in silicates by scanning transmission X-ray microscopy at the Fe L2,3 edges. Contributions to Mineralogy and Petrology, 166, p. 423-434. doi:10.1007/s00410-013-0883-4.

De Andrade V., Ganne J., Dubacq B., Ryan C.G., Bourdelle F., Plunder A., Falkenberg G. and Thieme J. (2014). – Retrieving past geodynamic events by unlocking rock archives with μ-XRF and μ-spectroscopy. Journal of Physics: Conference Series, 499, 012012. doi :10.1088/1742-6596/499/1/012012.

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Techniques, méthodes et outils pour la quantification du métamorphisme (N. Riel et P. Lanari)

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Lanari P., Vidal O., De Andrade V., Dubacq B., Lewin E., Grosch E. G. & Schwartz S. (2014). – XMapTools: A MATLAB©-based program for electron microprobe X-ray image processing and geothermobarometry. Computers and Geosciences, 62, p. 227-240.

 

Dater les événements métamorphiques : exemple du chronomètre Th-U-Pb dans la monazite (A. Didier & V. Bosse)

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Didier A., Bosse V., Boulvais P., Bouloton J., Paquette J.L., Montel J.M., Devidal J.L. (2013). – Disturbance versus preservation of U–Th–Pb ages in monazite during fluid–rock interaction: textural, chemical and isotopic in situ study in microgranites (Velay Dome, France). Contrib. Mineral. Petrol. 165, p. 1051-1072.

Didier A., Bosse V., Cherneva Z., Gautier P., Georgieva M., Paquette J.L., Gerdjikov I. (2014). – Syn-deformation fluid-assisted growth of monazite during renewed high-grade metamorphism in metapelites of the Central Rhodope (Bulgaria, Greece). Chem. Geol.381, p. 206-222.

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Les marqueurs des évaporites dans la formation des gemmes métamorphiques ( G. Giuliani et al.)

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Cheilletz A., Féraud G., Giuliani G., Rodriguez C.T. (1994). – Time-pressure-temperature formation of Colombian emerald: an 40Ar/39Ar laser-probe and fluid inclusion-microthermometry contribution. Economic Geology, 89, p. 361-380.

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Feneyrol J., Ohnenstetter D., Giuliani G., Fallick A.E., Rollion-Bard Cl., Robert J.-L., Malisa E. (2012). – Evidence of evaporites in the genesis of the vanadian grossular 'tsavorite' deposit in Namalulu, Tanzania. Canadian Mineralogist, 50, p. 745-769.

Feneyrol J., Giuliani G., Ohnenstetter D., Fallick A.E., Martelat J.M., Monié P., Dubessy C., Rollion-Bard Cl., Le Goff E., Malisa E., Rakotondrazafy A.F.M., Pardieu V., Kahn T., Ichang'i, D., Venance E., Voarintsoa N.R., Ranatsenho M., Simonet C., Omito E., Nyamai C., Saul M. (2013). – Worldwide tsavorite deposits: new aspects and perspectives. Ore Geology Reviews, 53, p. 1-25.

Garnier V., Ohnenstetter D., Giuliani G. (2004). – L'aspidolite fluorée : rôle des évaporites dans la genèse des marbres de Nangimali (Azad-Kashmir, Pakistan). C.R. Géosciences, 336, p. 1245-1253.

Garnier V., Giuliani G., Ohnenstetter D., Fallick A.E., Dubessy J., Banks D., Hoàng Quang V., Lhomme Th., Maluski H., Pêcher A., Bakhsh K.A., Pham Van L., Phan Trong T., Schwarz D. (2008). – Marble-hosted ruby deposits from central and Southeast Asia: towards a new genetic model. Ore Geology Reviews, 34, p. 169-191.

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Giuliani G., France-Lanord Ch., Cheilletz A., Coget P., Branquet Y., Laumonier B. (2000). – Sulfate reduction by organic matter in Colombian emerald deposits: chemical and stable isotope (C, O, H) evidence. Economic Geology, 95, p. 1129-1153.

Giuliani G., Dubessy J., Banks D., Hoang Quang V., Lhomme T., Pironon J., Garnier, V., Phan Trong T., Pham Van L., Ohnenstetter D., Schwarz D. (2003). – CO2-H2S-COS-S8-AlO(OH)-bearing fluid inclusions in ruby from marble-hosted deposits in Luc Yen area, North Vietnam. Chemical Geology, 194, p. 167-185.

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Pokrovski G.S., Dubrovinsky L.S. (2011). – The S3- ion is stable in geological fluids at elevated temperatures and pressures. Science, 331, p. 1052-1054.

Pokrovski G.S., Dubessy J. (2014). – Stability and abundance of the trisulfur radical ion S3- in hydrothermal fluids. Earth and Planetary Science Letters, 411, p. 298-309.

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Piégeage et libération des halogènes dans les métagabbros océaniques ( C. Nicollet et F. Cattani)

Coogan L.A., Wilson R.N., Gills K.M. and MacLeod C.J. (2001). – Nearsolidus evolution of oceanic gabbros: Insights from amphibole geochemistry. Geochimica and Cosmochimica Acta, 65, p. 4339-4357.

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Rôle des fluids dans le métamorphisme (Ph. Goncalves et C. Durand)

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Oliot E. et al. (2010). – Role of plagioclase and reaction softening in a metagranite shear zone at mid-crustal conditions (Gotthard Massif, Swiss Central Alps). Journal of Metamorphic Geology, 28, p. 849-871.

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