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The subduction plate interface: rock record and mechanical coupling (from long to short timescales)

Lithos, 2018-11, Vol.320-321, p.537-566

2018

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Plate interface rheological switches during subduction infancy: Control on slab penetration and metamorphic sole formation

Earth and planetary science letters, 2016-10, Vol.451, p.208-220

2016

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Exhumation of oceanic blueschists and eclogites in subduction zones: Timing and mechanisms

Earth-science reviews, 2009, Vol.92 (1), p.53-79

2009

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Zagros orogeny: a subduction-dominated process

Geological magazine, 2011-11, Vol.148 (5-6), p.692-725

2011

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Initial water budget: The key to detaching large volumes of eclogitized oceanic crust along the subduction channel?

Lithos, 2010-12, Vol.120 (3), p.453-474

2010

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Convergence history across Zagros (Iran): constraints from collisional and earlier deformation

International journal of earth sciences : Geologische Rundschau, 2005-07, Vol.94 (3), p.401-419

2005

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Slabitization: Mechanisms controlling subduction development and viscous coupling

Earth-science reviews, 2020-09, Vol.208, p.103259, Article 103259

2020

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Mantle Wedge (De)formation During Subduction Infancy: Evidence from the Base of the Semail Ophiolitic Mantle

Journal of petrology, 2018-11, Vol.59 (11), p.2061-2092

2018

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No large earthquakes in fully exposed subducted seamount

Geology (Boulder), 2019-05, Vol.47 (5), p.407-410

2019

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Eclogite breccias in a subducted ophiolite: A record of intermediate-depth earthquakes?

Geology (Boulder), 2012-08, Vol.40 (8), p.707-710

2012

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Buildup of a dynamically supported orogenic plateau: Numerical modeling of the Zagros/Central Iran case study

Geochemistry, geophysics, geosystems : G3, 2014-06, Vol.15 (6), p.2632-2654

2014

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Eclogitization of the Monviso ophiolite (W. Alps) and implications on subduction dynamics

Journal of metamorphic geology, 2012-01, Vol.30 (1), p.37-61

2012

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True metamorphic isograds or tectonically sliced metamorphic sequence? New high-spatial resolution petrological data for the New Caledonia case study

Contributions to mineralogy and petrology, 2013-08, Vol.166 (2), p.451-469

2013

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Timescales of subduction initiation and evolution of subduction thermal regimes

Earth and planetary science letters, 2022-04, Vol.584, p.117521, Article 117521

2022

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The Zermatt-Saas ophiolite: the largest (60-km wide) and deepest (c. 70-80 km) continuous slice of oceanic lithosphere detached from a subduction zone?

Terra nova (Oxford, England), 2009-06, Vol.21 (3), p.171-180

2009

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A 3-D crustal shear wave velocity model and Moho map below the Semail Ophiolite, eastern Arabia

Geophysical journal international, 2022-07, Vol.231 (2), p.817-834

2022

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Fluid Pulses During Stepwise Brecciation at Intermediate Subduction Depths (Monviso Eclogites, W. Alps): First Internally Then Externally Sourced

Geochemistry, geophysics, geosystems : G3, 2019-11, Vol.20 (11), p.5285-5318

2019

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Fluid‐Assisted Deformation and Strain Localization in the Cooling Mantle Wedge of a Young Subduction Zone (Semail Ophiolite)

Journal of Geophysical Research, 2018-09, Vol.123 (9), p.7529-7549

2018

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Evidence for Paleocene–Eocene evolution of the foot of the Eurasian margin (Kermanshah ophiolite, SW Iran) from back-arc to arc: Implications for regional geodynamics and obduction

Lithos, 2013-12, Vol.182-183, p.11-32

2013

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Subduction interface processes recorded by eclogite-facies shear zones (Monviso, W. Alps)

Lithos, 2011-11, Vol.127 (1-2), p.222-238

2011

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Effect of fluid circulation on subduction interface tectonic processes: Insights from thermo-mechanical numerical modelling

Earth and planetary science letters, 2012-12, Vol.357-358, p.238-248

2012

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Transient, synobduction exhumation of Zagros blueschists inferred from P-T, deformation, time, and kinematic constraints: Implications for Neotethyan wedge dynamics

Journal of Geophysical Research - Solid Earth, 2006-11, Vol.111 (B11), p.B11401-n/a

2006

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Fossil seamount in southeast Zagros records intraoceanic arc to back-arc transition: New constraints for the evolution of the Neotethys

Gondwana research, 2020-05, Vol.81, p.423-444

2020

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Coeval blueschist exhumation along thousands of kilometers: Implications for subduction channel processes

Geochemistry, geophysics, geosystems : G3, 2009-07, Vol.10 (7), p.Q07002-n/a

2009

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How continuous and precise is the record of P-T paths? Insights from combined thermobarometry and thermodynamic modelling into subduction dynamics (Schistes Lustrés, W. Alps)

Journal of metamorphic geology, 2012-04, Vol.30 (3), p.323-346

2012

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The subduction plate interface: rock record and mechanical coupling (from long to short timescales)

Plate interface rheological switches during subduction infancy: Control on slab penetration and metamorphic sole formation

Exhumation of oceanic blueschists and eclogites in subduction zones: Timing and mechanisms

Zagros orogeny: a subduction-dominated process

Initial water budget: The key to detaching large volumes of eclogitized oceanic crust along the subduction channel?

Convergence history across Zagros (Iran): constraints from collisional and earlier deformation

Slabitization: Mechanisms controlling subduction development and viscous coupling

Mantle Wedge (De)formation During Subduction Infancy: Evidence from the Base of the Semail Ophiolitic Mantle

No large earthquakes in fully exposed subducted seamount

Eclogite breccias in a subducted ophiolite: A record of intermediate-depth earthquakes?

Buildup of a dynamically supported orogenic plateau: Numerical modeling of the Zagros/Central Iran case study

Eclogitization of the Monviso ophiolite (W. Alps) and implications on subduction dynamics

True metamorphic isograds or tectonically sliced metamorphic sequence? New high-spatial resolution petrological data for the New Caledonia case study

Timescales of subduction initiation and evolution of subduction thermal regimes

The Zermatt-Saas ophiolite: the largest (60-km wide) and deepest (c. 70-80 km) continuous slice of oceanic lithosphere detached from a subduction zone?

A 3-D crustal shear wave velocity model and Moho map below the Semail Ophiolite, eastern Arabia

Fluid Pulses During Stepwise Brecciation at Intermediate Subduction Depths (Monviso Eclogites, W. Alps): First Internally Then Externally Sourced

Fluid‐Assisted Deformation and Strain Localization in the Cooling Mantle Wedge of a Young Subduction Zone (Semail Ophiolite)

Evidence for Paleocene–Eocene evolution of the foot of the Eurasian margin (Kermanshah ophiolite, SW Iran) from back-arc to arc: Implications for regional geodynamics and obduction

Subduction interface processes recorded by eclogite-facies shear zones (Monviso, W. Alps)

Effect of fluid circulation on subduction interface tectonic processes: Insights from thermo-mechanical numerical modelling

Transient, synobduction exhumation of Zagros blueschists inferred from P-T, deformation, time, and kinematic constraints: Implications for Neotethyan wedge dynamics

Fossil seamount in southeast Zagros records intraoceanic arc to back-arc transition: New constraints for the evolution of the Neotethys

Coeval blueschist exhumation along thousands of kilometers: Implications for subduction channel processes

How continuous and precise is the record of P-T paths? Insights from combined thermobarometry and thermodynamic modelling into subduction dynamics (Schistes Lustrés, W. Alps)

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