Formation of Olivine Veins by Reactive Fluid Flow in a Dehydrating Serpentinite

Thermolab: A Thermodynamics Laboratory for Nonlinear Transport Processes in Open Systems

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Field‐based evidence for intra‐slab high‐permeability channel formation at eclogite‐facies conditions during subduction

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Instantaneous rock transformations in the deep crust driven by reactive fluid flow

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Seismically-induced serpentine dehydration as a possible mechanism of water release in subduction zones. Insights from the Alpine Corsica pseudotachylyte-bearing Monte Maggiore ophiolitic unit

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The role of the antigorite + brucite to olivine reaction in subducted serpentinites (Zermatt, Switzerland)

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Metamorphic olivine after dehydration embrittlement in Serpentinite: Case study from the Shiraga Serpentinite mass in the Sanbagawa high P/T metamorphic belt, central Shikoku, Japan

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Resolving hydro-mechanical coupling in two and three dimensions: Spontaneous channelling of porous fluids owing to decompaction weakening

(2019) L Räss et al.   GEOPHYSICAL JOURNAL INTERNATIONAL

Molybdenum systematics of subducted crust record reactive fluid flow from underlying slab serpentine dehydration

(2019) Shuo Chen et al.   Nature Communications

Tracing dehydration and melting of the subducted slab with tungsten isotopes in arc lavas

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Interplay between fluid extraction mechanisms and antigorite dehydration reactions (Val Malenco, Italian Alps)

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Fluid migration in the mantle wedge: Influence of mineral grain size and mantle compaction

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Fluid–rock interaction and evolution of a high-pressure/low-temperature vein system in eclogite from New Caledonia: insights into intraslab fluid flow processes

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Dehydration-induced porosity waves and episodic tremor and slip

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Isotopic evidence for iron mobility during subduction

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Role of iron content on serpentinite dehydration depth in subduction zones: Experiments and thermodynamic modeling

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Fluid escape from subduction zones controlled by channel-forming reactive porosity

(2016) Oliver Plümper et al.   Nature Geoscience

Coupling changes in densities and porosity to fluid pressure variations in reactive porous fluid flow: Local thermodynamic equilibrium

(2015) Benjamin Malvoisin et al.   GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS

Fluid flow in subduction zones: The role of solid rheology and compaction pressure

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Channelized Fluid Flow and Eclogite-facies Metasomatism along the Subduction Shear Zone

(2014) Samuel Angiboust et al.   JOURNAL OF PETROLOGY

Petrology and Trace Element Budgets of High-pressure Peridotites Indicate Subduction Dehydration of Serpentinized Mantle (Cima di Gagnone, Central Alps, Switzerland)

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Pathway from subducting slab to surface for melt and fluids beneath Mount Rainier

(2014) R. Shane McGary et al.   NATURE

Locking of the Chile subduction zone controlled by fluid pressure before the 2010 earthquake

(2014) Marcos Moreno et al.   Nature Geoscience

Tschermak's substitution in antigorite and consequences for phase relations and water liberation in high-grade serpentinites

(2013) José Alberto Padrón-Navarta et al.   LITHOS

Evidence for channelized external fluid flow and element transfer in subducting slabs (Raspas Complex, Ecuador)

(2012) Petra Herms et al.   CHEMICAL GEOLOGY

The role of serpentinites in cycling of carbon and sulfur: Seafloor serpentinization and subduction metamorphism

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Episodic tremor and slow slip potentially linked to permeability contrasts at the Moho

(2012) Ikuo Katayama et al.   Nature Geoscience

Volcanic arcs fed by rapid pulsed fluid flow through subducting slabs

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Compaction-dissolution waves in an upwelling mantle column

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Subduction factory: 4. Depth-dependent flux of H2O from subducting slabs worldwide

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Internal and External Fluid Sources for Eclogite-facies Veins in the Monviso Meta-ophiolite, Western Alps: Implications for Fluid Flow in Subduction Zones

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Fluid transfer into the wedge controlled by high-pressure hydrofracturing in the cold top-slab mantle

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Breakdown mechanisms of titanclinohumite in antigorite serpentinite (Cerro del Almirez massif, S. Spain): A petrological and TEM study

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Trace-element mobilization in slabs due to non steady-state fluid–rock interaction: Constraints from an eclogite-facies transport vein in blueschist (Tianshan, China)

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