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| 1 | Eclogitic metasediments from the Tso Morari area (Ladakh, Himalaya): Evidence for continental subduction during India-Asia convergence显示文摘 | GuiUot S de Sigoyer J Lardeaux J M | 1997 | Contributions to Mineralogy and Petrology1997，128，： | 1 |
| 2 | Glaucophane-bearing eclogites m the Tso Morari dome (eastern Ladakh, NW Himalaya)显示文摘 | de Sigoyer J Guillot S Lardeaux J M | 1997 | Eurapean Journal of Mineralogy1997，9，： | 1 |
| 3 | The Variscan French Massif Central-a new addition to the ultra-high pressure metamorphic 'club':exhumation processes and geodynamic consequences显示文摘 | Lardeaux J M Ledru P Daniel I Duchene S | | 0，，： | 1 |
| 4 | Kinetics of the coesite-quartz transition:application to the exhumation of ultrahigh-pressure rocks显示文摘 | Perrillat J P Daniel I Lardeaux J M Cardon H | | 0，，： | 1 |
| 5 | The Lu-Hf dating of garnets and the ages of the Alpine high-pressure metamorphism 显示文摘 | Duch~ne S Blichert-Toft J Luais B T~louk Lardeaux J M | 1997 | Nature1997，387，6633： | 1 |
| 6 | The Lu-Hf dating of garnets and the ages of the Alpine high-pressure metamorphism 显示文摘 | Duchene S Blichert-Toft J Luais B Telouk P Lardeaux J-M | 1997 | Nature1997，387，6633： | 1 |
| 7 | Evolution of the East African and related orogens, and the assembly of Gondwana显示文摘 | Goncalves P Nieollet C Jean-Marc Lardeaux J M | 2003 | Precambrian Research2003，12，234： | 1 |
| 8 | Finite strain patterns in Andriamena unit (north-central Madagascar ): Evidence for late Neopmterozoic-Cambrian thrusting during continental convergence 显示文摘 | Goncalves P Nicollet C Lardeaux J M | 2003 | Precambrian Research2003，123，： | 1 |
| 9 | Deformation and recrystallization mechanisms in naturally deformed omphacite from the SesiaLanzo zone显示文摘 | Buatier M Van Roermund H.L.M Drury M.R Lardeaux J. M | | 0，，： | 1 |
| 10 | Metamorphism and tectonics in southern Madagascar: an overview显示文摘 | J M Lardeaux | 1999 | Gondivana Research1999，2，3： | 1 |
| 11 | Modification of antiphase domain sizes in omphacite by dislocation glide and creep mechanisms and its petrological consequences显示文摘 | Van Roermund H L M Lardeaux J. M | | 0，，： | 1 |
| 12 | A new discovery of eclogites from the Himalaya,Tso Morari dome unit(northwestern India) 显示文摘 | Guillot S Mascle G Lardeaux J M | 1995 | Mitteilungen des Geologischen Institut ETH Zurich und Universitat Zurich Neue Folge1995，298，： | 1 |
| 13 | Lithospheric tectonic structures developed under high-grade metamorphism in the southern part of Madagascar显示文摘 | Martelat J E Nicollet C Lardeaux J M | 1997 | Geodin- Acta1997，，10： | 1 |
| 14 | A relict blueschist in meta-ophiolite from the central Norwegian Caledonides—discovery and consequences显示文摘 | E.A Eide J.-M Lardeaux | 2002 | LITHOS2002，，1： | 1 |
| 15 | Eclogitic Metasediments from the Tso Morari Area(Ladakh,Himalaya):Evidence for Continental Subduction during India-Asia Convergence显示文摘 | Guillot S de Sigoyer J Lardeaux J M | 1997 | Contributions to Mineralogy and Petrology1997，128，： | 1 |
| 16 | Mineral zoning and exhumation history in the Mü nchberg eclogites (Bohemia)显示文摘 | Duchê ne S Albarè de F Lardeaux J M | 1998 | Am J Sci1998，298，： | 1 |
| 17 | How many subductions in the Variscan orogeny?Insights from numerical models显示文摘We developed a 2 D numerical model to simulate the evolution of two superposed ocean-continent-ocean subduction cycles with opposite vergence,both followed by continental collision,aiming to better understand the evolution of the Variscan belt.Three models with different velocities of the first oceanic subduction have been implemented.Striking differences in the thermo-mechanical evolution between the first subduction,which activates in an unperturbed system,and the second subduction,characterised by an opposite vergence,have been enlighten,in particular regarding the temperature in the mantle wedge and in the interior of the slab.Pressure and temperature(P-T) conditions predicted by one cycle and two cycles models have been compared with natural P-T estimates of the Variscan metamorphism from the Alps and from the French Massif Central(FMC).The comparative analysis supports that a slow and hot subduction well reproduces the P-T conditions compatible with data from the FMC,while P-T conditions compatible with data of Variscan metamorphism from the Alps can be reproduced by either a cold or hot oceanic subduction models.Analysing the agreement of both double and single subduction models with natural P-T estimates,we observed that polycyclic models better describe the evolution of the Variscan orogeny. | Alessandro Regorda Jean-Marc Lardeaux Manuel Roda Anna Maria Marotta Maria Iole Spalla | 2020 | Geoscience Frontiers2020，11，3： | 0 |
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