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| 1 | Reactive and viscous flow in hypersonic nozzles显示文摘 | ZEITOUN D BOCCACIO E DRUGUET M C IMBERT M | 1994 | AIAA Journal1994，32，2： | 1 |
| 2 | Effect of numerics on Navier-Stokes computations of hypersonic double-cone flows显示文摘 | Druguet M C | 2005 | AIAA Journal2005，43，3： | 1 |
| 3 | Numerical modeling of asymmetricboudinage显示文摘 | Passchier C W Druguet E | 2002 | Journal of Structural Geology2002，24，11： | 1 |
| 4 | Prediction of the flow field over an orbiter entering the Mars atmosphere显示文摘 | DRUGUET M C | 2010 | Shock Waves2010，20，3： | 1 |
| 5 | Reactive and viscous flowin hypersonic nozzles显示文摘 | ZEITOUN D BOCCACCIO E DRUGUET M C | 1994 | AIAA Journal1994，32，2： | 1 |
| 6 | An extension of CVDV model to Zeldovich exchange reactions for hypersonic non-equilibrium air flows显示文摘 | S. Séror E. Schall M.-C. Druguet D.E. Zeitoun | 1998 | Shock Waves1998，，5： | 1 |
| 7 | Multidimensional dissipation for upwind schemes: stability and applications to gas dynamics 显示文摘 | Sanders R Morano E Druguet M C | 1998 | Journal of Computational Physics1998，145，2： | 1 |
| 8 | Prediction of the flow field over an orbiter entering the Mars atmosphere显示文摘 | Druguet M C | 2010 | Shock Waves2010，20，： | 1 |
| 9 | Effect of numerics on navier-stokes computations of hypersonic double-cone flows显示文摘 | | 2005 | AIAA Journal2005，43，3： | 1 |
| 10 | Apparent boudinage in dykes显示文摘 | Bons P D Druguet E Haman I | 2004 | Journal of Structural Geology2004，26，： | 1 |
| 11 | Prediction of the flow field over an orbiter entering the Mars atmosphere显示文摘 | Druguet M-C | | 0，，： | 1 |
| 12 | Effect of numerics on Navier-Stokes computations of hypersonic double-cone显示文摘 | Druguet Made Claude | | AIAA0，43，3： | 1 |
| 13 | Effect of numerics on Navier-Stokes computations of hypersonic double-cone flows显示文摘 | Druguet M Candler G V Nompelis I | 2005 | AIAA Journal2005，43，3： | 1 |
| 14 | Shear zone-related fold显示文摘 | Carreras J Druguet E Albert G | 2005 | Journal of Structural Geology2005，27，： | 1 |
| 15 | Numerical modeling of asymmetric boudinage显示文摘 | Druguet E | 2002 | Journal of Structural Geology2002，24，： | 1 |
| 16 | Reactive and viscous flow in hypersonic nozzles显示文摘 | Zeitoun D Boccaccio E Druguet M C | 1994 | AIAA Journal1994，32，2： | 1 |
| 17 | Effect of numeric on Navier-Stokes computation of hypersonic double-cone flows 显示文摘 | Druguet M C Candler G V Nompelis 1 | 2005 | AIAA Journal2005，43，3： | 1 |
| 18 | Multidimensional dissipation for upwind schemes:stability and applications to gas dynamics 显示文摘 | Sanders R Morano E Druguet M C | 1998 | J Comput Phys1998，145，2： | 1 |
| 19 | Deciphering the presence of axial-planar veins in tectonites显示文摘Veins and dikes are often oriented subparallel to the axial surfaces of folds in the adjacent layered or foliated rocks.This implies an awkward situation,since veins would lay in planes close-to-parallel to the maximum stretching axis.A series of geometric models have been conceived in order to gain insight into the possible mechanisms for their formation.The models are based on the analysis of a varied selection of field structures and on the review of similar structures in the existing literature.A first categorization consists on distinguishing between axial-planar veins achieved by either progressive or polyphase deformation.Five models of axial-planar veins resulting from progressive deformation are described and discussed:(1) fold-related veins associated with the standard folding mechanisms,(2) fracture arrays localized along the short limbs of folds(asymmetric fold-related veins),(3) folds associated with rotation of extension veins(vein-related folds),(4) high strain and transposition of early veins,and(5) high strain and late veins parallel to axial planar foliations(axial planar foliation-related veins).The axial planar geometry is achieved through variable amounts of progressive rotational strain,except in model 5,in which the co-planarity is acquired at the time of vein intrusion.The possibility for axial-planar veins to have developed in two distinct phases in the context of polyphase or polyorogenic tectonics has also been explored and discussed.This study contributes to a better understanding of the intriguing interplays between deformation,metamorphic and magmatic processes in orogenic belts. | Elena Druguet | 2019 | Geoscience Frontiers2019，10，6： | 0 |
| 20 | Early Paleozoic accretionary orogens along the Western Gondwana margin显示文摘Early Paleozoic accretionary orogens dominated the Western Gondwana margin and were characterized by nearly continuous subduction associated with crustal extension and back-arc basin development.The southwestern margin is represented by Famatinian and Pampean basement realms exposed in South America,both related to the protracted Paleozoic evolution of the Terra Australis Orogen,whereas the northwestern margin is mainly recorded in Cadomian domains of Europe and adjacent regions.However,no clear relationships between these regions were so far established.Based on a compilation and reevaluation of geological,paleomagnetic,petrological,geochronological and isotopic evidence,this contribution focuses on crustal-scale tectonic and geodynamic processes occurring in Western Gondwana accretionary orogens,aiming at disentangling their common Early Paleozoic evolution.Data show that accretionary orogens were dominated by high-temperature/lowpressure metamorphism and relatively high geothermal gradients,resulting from the development of extended/hyperextended margins and bulk transtensional deformation.In this sense,retreating-mode accretionary orogens characterized the Early Paleozoic Gondwana margin,though short-lived pulses of compression/transpression also occurred.The existence of retreating subduction zones favoured mantle-derived magmatism and mixing with relatively young(meta)sedimentary sources in a thin continental crust.Crustal reworking of previous forearc sequences due to trenchward arc migration thus took place through assimilation and anatexis in the arc/back-arc regions.Therefore,retreating-mode accretionary orogens were the locus of Early Paleozoic crustal growth in Western Gondwana,intimately associated with major flare-up events,such as those related to the Cadomian and Famatian arcs.Slab roll back,probably resulting from decreasing convergence rates and plate velocities after Gondwana assembly,was a key factor for orogen-scale geodynamic processes.Coupled with synchronous oblique subduction and crustal-scale dextral deformation,slab roll back might trigger toroidal mantle flow,thus accounting for bulk dextral transtension,back-arc extension/transtension and a large-scale anticlockwise rotation of Gondwana mainland. | Sebastián Oriolo Bernhard Schulz Silvana Geuna Pablo DGonzález Juan E.Otamendi JiíSláma Elena Druguet Siegfried Siegesmund | 2021 | Geoscience Frontiers2021，12，1： | 0 |
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