59 results on '"Angiboust, Samuel"'
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2. Multiple sulfur isotopes evidence deep intra-slab transport of sulfate-rich fluids
3. The B isotopic signature of serpentine from obducted ophiolites: Mixing of fluids and tectonic implications
4. Garnet fracturing reveals ancient unstable slip events hosted in plate interface metasediments
5. Fluids in the Earth's lithosphere: From petrology to geodynamics
6. Accretion and subduction mass transfer processes: Zircon SHRIMP and geochemical insights from the Carboniferous Western Series, Central Chile
7. The B isotopic signature of serpentine from Supra Subduction Zone ophiolites: mixing of fluids and tectonic implications.
8. Arrested decarbonation in an ancient subduction zone: Isotopic and petrographic evidence from HP/UHP meta-ophiolitic breccias in the Western Alps
9. Cretaceous thermal evolution of the closing Neo-Tethyan realm revealed by multi-method petrochronology
10. Permeability of subducted oceanic crust revealed by eclogite-facies vugs
11. Supplemental Material: Permeability of subducted oceanic crust revealed by eclogite-facies vugs
12. Supplemental Material: Permeability of subducted oceanic crust revealed by eclogite-facies vugs
13. Episodic fluid flow in an eclogite-facies shear zone: Insights from Li isotope zoning in garnet
14. The rise and demise of deep accretionary wedges: A long-term field and numerical modeling perspective
15. Blueschist-facies paleo-earthquakes in a serpentinite channel (Zagros suture, Iran) enlighten seismogenesis in Mariana-type subduction margins
16. Jolts in the Jade factory: A route for subduction fluids and their implications for mantle wedge seismicity
17. Effective rheology of a two-phase subduction shear zone: Insights from numerical simple shear experiments and implications for subduction zone interfaces
18. Episodic hydrofracturing and large-scale flushing along deep subduction interfaces: Implications for fluid transfer and carbon recycling (Zagros Orogen, southeastern Iran)
19. Effective rheology of a two-phase subduction shear zone: insights from numerical simple shear experiments and implications for subduction zone interfaces
20. Large-scale fluid circulation in deep subduction interfaces: implications on fast and slow earthquake-related processes
21. Accretion-controlled forearc deformation pulses recorded by high-pressure paleo-accretionary wedges: the example of the Hellenic subduction zone
22. The Zagros Suture Amphibolites Record the Cretaceous Thermal Evolution of the Closing Tethyan Realm
23. Assessing sulfur sources and pyrite precipitation during eclogite-facies intra-slab fluid-flow (Monviso Lower Shear Zone, W. Alps)
24. Fluid and mass transfer along transient subduction interfaces in a deep paleo-accretionary wedge (Western Alps)
25. The boron isotopic signature of serpentine from obducted ophiolites: mixture of fluids and tectonic implications.
26. Drainage of subduction interface fluids into the forearc mantle evidenced by a pristine jadeitite network (Polar Urals)
27. Petrochronological close-up on the thermal structure of a paleo-subduction zone (W. Alps)
28. Deep mantle serpentinization in subduction zones: Insight from in situ B isotopes in slab and mantle wedge serpentinites
29. Multiple veining in a paleo–accretionary wedge: The metamorphic rock record of prograde dehydration and transient high pore-fluid pressures along the subduction interface (Western Series, central Chile)
30. Transient stripping of subducting slabs controls periodic forearc uplift
31. Fore-arc building and destruction: a critical interplay between fluid flow, megathrust strength and tectonic underplating
32. Effective rheology of a two-phase subduction shear zone calculated by numerical simple shear experiments
33. Squeezed Under the Sheet: White Mica Records High Tectonic Stresses Within a Decollement Thrust
34. The Fate of Subduction Fluids above the Subduction Interface: Implications for Mantle Wedge Deformation Processes
35. Exhumation of eclogitic ophiolitic nappes in the W. Alps: New age data and implications for crustal wedge dynamics
36. Deformation along the roof of a fossil subduction interface in the transition zone below seismogenic coupling: The Austroalpine case and new insights from the Malenco Massif (Central Alps)
37. Scales of fluid-rock interaction and carbon mobility in the deeply underplated and HP-Metamorphosed Schistes Lustrés, Western Alps
38. Fingerprinting and relocating tectonic slices along the plate interface: Evidence from the Lago Superiore unit at Monviso (Western Alps)
39. Middle to Late Miocene Age for the End of Amphibolite‐Facies Mylonitization of the Alpine Schist, New Zealand: Implications for Onset of Transpression Across the Alpine Fault
40. Stress-driven fluid flow controls long-term megathrust strength and deep accretionary dynamics
41. Deformation-enhanced fluid and mass transfer along Western and Central Alps paleo-subduction interfaces: Significance for carbon cycling models
42. Field report: Sailing around the exhumed roots of the Mesozoic Patagonian paleo-accretionary wedge (Diego de Almagro Island, Chile)
43. Brittle deformation during Alpine basal accretion and the origin of seismicity nests above the subduction interface
44. Rehydration of eclogites and garnet-replacement processes during exhumation in the amphibolite facies
45. A 100-m.y.-long window onto mass-flow processes in the Patagonian Mesozoic subduction zone (Diego de Almagro Island, Chile)
46. review of Giuntoli et al. paper
47. Ilmenite breakdown and rutile-titanite stability in metagranitoids: Natural observations and experimental results
48. Evidence for brittle deformation events at eclogite-facies P-T conditions (example of the Mt. Emilius klippe, Western Alps)
49. Hot subduction in the middle Jurassic and partial melting of oceanic crust in Chilean Patagonia
50. Eclogite-, amphibolite- and blueschist-facies rocks from Diego de Almagro Island (Patagonia): Episodic accretion and thermal evolution of the Chilean subduction interface during the Cretaceous
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