Thomas P. Ferrand
Thomas P. Ferrand
Scripps Institution of Oceanography, UC San Diego
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Dehydration-driven stress transfer triggers intermediate-depth earthquakes
TP Ferrand, N Hilairet, S Incel, D Deldicque, L Labrousse, J Gasc, ...
Nature communications 8 (1), 1-11, 2017
Laboratory earthquakes triggered during eclogitization of lawsonite-bearing blueschist
S Incel, N Hilairet, L Labrousse, T John, D Deldicque, T Ferrand, Y Wang, ...
Earth and Planetary Science Letters 459, 320-331, 2017
Impact of stylolites on the mechanical strength of limestone
P Baud, A Rolland, M Heap, T Xu, M Nicolé, T Ferrand, T Reuschle, ...
Tectonophysics 690, 4-20, 2016
Faulting of natural serpentinite: Implications for intermediate-depth seismicity
J Gasc, N Hilairet, T Yu, T Ferrand, A Schubnel, Y Wang
Earth and Planetary Science Letters 474, 138-147, 2017
Energy balance from a mantle pseudotachylyte, Balmuccia, Italy
TP Ferrand, L Labrousse, G Eloy, O Fabbri, N Hilairet, A Schubnel
Journal of Geophysical Research: Solid Earth 123 (5), 3943-3967, 2018
Physical mechanisms of oceanic mantle earthquakes: Comparison of natural and experimental events
S Kita, TP Ferrand
Scientific reports 8 (1), 1-11, 2018
Seismicity and mineral destabilizations in the subducting mantle up to 6 GPa, 200 km depth
TP Ferrand
Lithos 334, 205-230, 2019
Reproduction expérimentale d'analogues de séismes mantelliques par déshydratation de l'antigorite & Comparaison à des pseudotachylites naturelles
T Ferrand
Neither antigorite nor its dehydration is “metastable”
TP Ferrand
American Mineralogist: Journal of Earth and Planetary Materials 104 (6), 788-790, 2019
Transition from amagmatic to volcanic margin: Mantle exhumation in the Vøring Basin before the Icelandic plume influence
TP Ferrand
Tectonophysics 776, 228319, 2020
Seismicity and mineral destabilizations in the subducting mantle as evidence of carbon and hydrogen transfer toward the deep Earth.
TP Ferrand
AGUFM 2019, MR41B-0058, 2019
Dehydration-driven stress transfer as a mechanism for lower Wadati-Benioff earthquakes
TP Ferrand, N Hilairet, S Incel, D Deldicque, L Labrousse, J Gasc, ...
GRAAL: Griggs-type Apparatus equipped with Acoustics in the Laboratory: a new instrument to explore the rheology of rocks at high pressure
R Champallier, J Precigout, Y Pinquier, TP Ferrand, S Incel, N Hilairet, ...
Seismic potential of antigorite-rich serpentinites, an experimental point of view
J Gasc, N Hilairet, Y Wang, T Yu, TP Ferrand, A Schubnel
High-pressure deformation experiments at ID06-LVP: in-situ measurements of stress partitioning within two-phases aggregates for understanding strain localisation in rocks
N Hilairet, TP Ferrand, S Merkel, P Raterron, A Schubnel, J Guignard, ...
Evaluation in-situ par rayonnement X synchrotron du partitionement des contraintes lors de la déformation sous haute pression et haute température d'agrégats minéralogiques …
N Hilairet, TP Ferrand, P Raterron, S Merkel, A Schubnel, J Guignard, ...
Deformation of two-phase polycrystals under high pressures: effect of phase proportions on in-situ textures and stress partitionning in olivine+ antigorite
N Hilairet, TP Ferrand, P Raterron, S Merkel, A Schubnel, J Guignard, ...
Influence de la quantité de serpentine sur la rhéologie de serpentinites et la sismicité des zones de subduction: expériences de déformation sous haute pression
N Hilairet, TP Ferrand, A Schubnel, S Merkel, J Guignard, J Gasc, ...
Laboratory earthquakes triggered by metamorphic reactions during the eclogitization of blueschist
S Incel, A Schubnel, N Hilairet, T John, L Labrousse, TP Ferrand, ...
Stress heterogeneities in-situ within deforming synthetic serpentinized peridotites.
N Hilairet, T Ferrand, A Schubnel, T Mandolini, S Merkel, P Raterron, ...
Geophysical Research Abstracts 21, 2019
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