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Research

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Publication list

  • Characterization of tectonic history and metamorphic evolution of exhumed High-Pressure ophiolites (W. Alps, Iran: Sistan, Zagros, Southern Chile; coll. J. Glodny, P. Agard, J. Omrani, T. Hyppolito, A. Garcia-Casco, P. Monié, A. Cambeses, B. Dragovic) 

  • Geochemistry of HP rocks and characterization of fluid circulation in subducted oceanic lithosphere (Coll. G. Bebout, J. Glodny, P.  Cartigny, C. Herviou, R. Mélis )

  • Experimental petrology using piston-cylinder apparatus (Coll. D. Harlov)

  • Deformation and microstructures within exhumed metamorphic terranes

  • Estimation of petrophysical properties of the subduction interface using seismic velocity anomalies

  • Thermo-mechanical modelling of exhumation processes in subduction channels (Coll. T. Gerya, A. Menant)    

  • Alexander Von Humboldt post-doctoral fellowship 2012-2013 : « Tracking intermediate-depth seismicity in fossilized subduction channels and constraints for  mechanical coupling at the plate interface » at the GFZ Potsdam (coll. O. Oncken)

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  • [63] Minnaert C., Angiboust S., Cambeses A., Glodny J., Muñoz-Montecinos J., Garcia-Casco A., Omphacitite formation and fluid-rock interaction processes in an intra-slab eclogite facies shear zone. Submitted.

  • [62] Muñoz-Montecinos J, Angiboust S, et al., Fluid-Driven Shear Instabilities in the Subducted Oceanic Mantle at Intermediate Depths: Insights from Western Alps meta-ophiolites. Submitted.

  • [61] Genot I, Angiboust S., Cartigny P., Multiple sulfur isotopes evidence deep intra-slab transport of sulfate-rich fluids (Monviso meta-ophiolite, W. Alps). In revision.

  • [60] Muñoz-Montecinos J, Angiboust S, Garcia-Casco A and Raimondo T. 2023. Metamorphic veins control brittle creep processes in the deep slow slip and tremor region. Tectonics 42(4).

  • [59] Martin C., Flores K, Harlow G, Angiboust S, Hodel F, Guice G. 2023. The B isotopic signature of serpentine from obducted ophiolites: mixing of fluids and tectonic implications. Lithos. 456: 107275.

  • [58] Angiboust S., Cambeses A, Fagereng A, et al. 2023. Fluids in the Earth's lithosphere: from petrology to geodynamics. Lithos special issue: 452, 107226. 10.1016/j.lithos.2023.107226

  • [57] Muñoz-Montecinos J, Cambeses A, Angiboust S. 2023. Accretion and subduction mass transfer processes: Zircon SHRIMP and geochemical insights from the Carboniferous Western Series, Central Chile. International geology reviews; https://doi.org/10.1080/00206814.2023.2185822

  • [56] Holtmann R, Muñoz-Montecinos J, Angiboust S, Cambeses A et al. 2022. Cretaceous thermal evolution of the closing Neo-Tethyan realm revealed by multi-method petrochronology. Lithos, 422, 106731.

  • [55] Angiboust S, Raimondo T. 2022. Permeability of subducted oceanic crust revealed by eclogite-facies vugs. Geology. 50 (8): 964–968. https://doi.org/10.1130/G50066.1

  • [54] Hoover W., Penniston-Dorland S…. Angiboust S & Agard P. 2022. Episodic fluid flow in an eclogite-facies shear zone: Insights from Li isotope zoning in garnet. Geology.

  • [53] Angiboust S, Muñoz-Montecinos J, Cambeses A, Raimondo T, Deldicque D, Garcia-Casco. 2021. Jolts in the Jade Factory: a route for subduction fluids and their implications for mantle wedge seismicity, Earth Science Reviews. 103720.

  • [52] Angiboust S, Menant A, Gerya T, Oncken O. 2021. The Rise and Demise of Deep Accretionary Wedges: A Long-Term Field and Numerical Modelling Perspective, Geosphere. 10.1130/GES02392.1

  • [51] Oncken O, Angiboust S, Dresen G, 2021. Slow slip in subduction zones: Reconciling deformation fabrics with instrumental observations and laboratory results, Geosphere. 10.1130/GES02382.1

  • [50] Muñoz-Montecinos J, Angiboust S, Garcia-Casco A, 2021. Blueschist-facies paleo-earthquakes in a serpentinite channel enlighten seismogenesis in Mariana-type subduction margins, Earth and Planetary Sciences Letters. 573, 117135.

  • [49] Muñoz-Montecinos J, Angiboust S, Garcia-Casco A, Glodny J and Bebout G., 2021. Episodic hydrofracturing and large-scale flushing along deep subduction interfaces: Implications for fluid transfer and carbon recycling, Chemical Geology. 120173 

  • [48] Ioannidi I, Le Pourhiet L, Agard P, Angiboust S, Oncken O., 2021. Effective rheology of a two-phase subduction shear zone: insights from numerical simple shear experiments and implications fo subduction zone interfaces, Earth and Planetary Sciences Letters. 566, 116913.

  • [47] Epstein G, Bebout G, Angiboust S., 2021. Fluid and mass transfer along transient subduction interfaces in a deep paleo-accretionary wedge (W. Alps). Chemical Geology, 119920.

  • [46] Angiboust S, Glodny J, Cambeses et al., 2021. Drainage of Subduction Interface Fluids into the Fore-arc Mantle Evidenced by a Pristine Jadeitite Network, Journal of Metamorphic Geology, 39, 473-500.

  • [45] Dragovic B, Angiboust S, Tappa M J., 2020. Petrochronological close-up on the thermal structure of a paleo-subduction zone (W.Alps). Earth and Planetary Sciences Letters, 547, 116446.

  • [44] Martin C, Flores K, Vitale-Brovarone A, Angiboust S, Harlow G.E, 2020. Deep mantle serpentinization in subduction zones: insight from in-situ B isotopes in slab and mantle wedge serpentinites. Chemical Geology, 119637 

  • [43] Menant A, Angiboust S, Gerya T, Lacassin R, Simoes M, Grandin R. 2020. Transient stripping of subducting slabs controls periodic forearc uplift. Nature Communications, 11:1823. 10.1038/s41467-020-15580-7.

  • [42] Muñoz-Montecinos J, Angiboust S, Cambeses A, Garcia-Casco A , 2020. Multiple veining in a paleo-accretionary wedge: The metamorphic rock record of prograde dehydration and transient high pore fluid pressures along the subduction interface (W. Series, central Chile). Geosphere. 10.1130/GES02227.1.

  • [41] Angiboust S & Glodny, 2020. J. Exhumation of Eclogitic Ophiolitic Nappes in the W. Alps: New Age Data and Implications for Crustal Wedge Dynamics . Lithos, 105374 .

  • [40] Bonnet G, Agard P, Fournier M, Whitechurch H, Angiboust S, Caron B. 2020. Fossil seamount in SE Zagros records intraoceanic arc to back-arc transition: new constraints for the evolution of the Neotethys. Gondwana Research. 81, 423-444. 10.1016/j.gr.2019.10.019. 

  • [39] Ioannidi P I, Angiboust S, Oncken O, Agard P, Glodny J, Sudo M, 2020. Deformation along the Roof of a Fossil Subduction Interface: the Austroalpine Case and New Insights from the Malenco Massif (Central Alps). Geosphere. 10.1130/GES02149.1 

  • [38] Gilio M, Scambelluri M, Agostini S, Godard M, Pettke T., Agard P., Locatelli M,  Angiboust S., 2020. Fingerprinting and relocating tectonic slices along the plate interface: evidence from the Lago Superiore Unit at Monviso (Western Alps). Lithos, 352, 105308.  10.1016/j.lithos.2019.105308 

  • [37] Epstein G, Bebout G ,  Angiboust S, Agard P.,  2020. Scales of fluid-rock interaction and carbon mobility in the deeply underplated and HP-metamorphosed Schistes Lustrés, Western Alps. Lithos. 105229. 10.1016/j.lithos.2019.105229 

  • [36] Ring U., Glodny J., Angiboust S., Little T., Lang K., 2019. Mid-Miocene age for amphibolite-facies metamorphism and mylonitization of the Alpine Schist, New Zealand: Implications for onset of transpression across the Alpine Fault . Tectonics. 38(12), 4335-4359.  10.1029/2019TC005577 

  • [35] Bonnet G., Agard P., Angiboust S., Monié P., Fournier M, Caron B., Omrani J.  2019 Structure and metamorphism of a subducted seamount (Zagros suture, S. Iran). Geosphere. https://doi.org/10.1130/GES02134.1 

  • [34] Yamato P, Duretz T & Angiboust S.  2019 Brittle/ductile deformation of eclogites: Insights from numerical models. Geochemistry Geophysics Geosystems. 20(7), 3116-3133.

  • [33] Menant A, Angiboust S, Gerya T.  2019 Stress-driven fluid flow controls megathrust strength and deep accretionary dynamics.  Scientific Reports. (9), 9714.

  • [32] Bonnet G., Agard P., Angiboust S., Fournier M, Omrani J.  2019. Seamounts do not trigger subduction mega-earthquakes. Geology. 47, 407-410. doi:10.1130/G45564.1 . 

  • [31] Agard P, Plunder A ,  Angiboust S, Bonnet G , Ruh J.,  2018. The subduction plate interface: rock record and mechanical coupling. Lithos. 320, 537-566 .

  • [30] Locatelli, M., Verlaguet A., Agard P., Federico L, and Angiboust S., 2018. Eclogite-facies rupture along the subduction plate interface (Monviso meta-ophiolite complex, W. Alps). Lithos. 320, 378-402.

  • [29] Angiboust S., Muñoz J., 2018. Field report: Sailing around the exhumed roots of the Mesozoic Patagonian paleo-accretionary wedge (Diego de Almagro Island, Chile).  Geoscience frontiers, 9, 1591-1594.

  • [28] Bonnet G., Agard, P, Angiboust S., Monié, P., Jentzer, M., Omrani, J. et al, 2018. Tectonic slicing and mixing processes along the subduction interface: close-up from the Sistan metamorphic suture (Eastern Iran). Lithos, 310, 269-287.

  • [27] Jaeckel, K., Bebout, G., Angiboust S., 2018. Deformation-Enhanced Fluid and Mass Transfer Along Western and Central  Alps Paleo-Subduction Interfaces: Significance for Carbon Cycling Models.  Geosphere, 14 (6), doi.org/10.1130/GES01587.1.

  • [26] Angiboust S., Cambeses, A., Hyppolito, T., Glodny, J., Monié, P. et al., 2018. A 100 Ma-long window onto accretionary processes in the Patagonian Mesozoic subduction zone (Diego de Almagro Island, Chile). GSA Bulletin, 130 (9-10): 1439-1456. 

  • [25] Hyppolito, T., Cambeses A., Angiboust S. et al., 2018. Rehydration of eclogites and garnet replacement processes  during exhumation in the amphibolite facies. Geological Soc. London Spec. Publications:  « Microscale to Mountain belts ». Eds. Ferrero, Grosch & Lanari.

  • [24] Menant, A., Angiboust S., Monié, P., Oncken, O., 2018. Brittle deformation during Alpine basal accretion and the origin of seismicity nests above the subduction interface. Earth and Planetary Science Letters, 487, 84-93.

  • [23] Angiboust, S. & Harlov, D. 2017c. Ilmenite breakdown and rutile – titanite stability in metagranitoids: natural observations and experimental results. American Mineralogist, 102.

  • [22] Hertgen S., Yamato P., Morales L. and Angiboust S., 2017. Evidence for brittle deformation events in the eclogite-facies (example of the Mt. Emilius klippe, W. Alps). Tectonophysics, 706, 1-13.

  • [21] Angiboust, S., Yamato P., Hertgen S., Hyppolito T., Bebout G. and Morales L., 2017b. Fluid pathways and high pressure metasomatism in a subducted continental slice (Mt. Emilius klippe, W. Alps).Journal of Metamorphic Geology, 35, 471-.

  • [20] Angiboust, S., Hyppolito, T., Glodny, J., Cambeses, A., Garcia-Casco, A., Calderon, M. & Juliani, C. 2017a. A hot subduction in the middle Jurassic and partial melting of oceanic crust in Chilean Patagonia. Gondwana Research, 42, 104-125.

  • [19] Hyppolito, T., Angiboust, S., Juliani, C., Glodny, J., Garcia-Casco, A., Calderon, M. & Chopin, C. 2016. 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. Lithos, 267, 422-440.

  • [18] Angiboust, S., Agard, P., Glodny, J., Omrani, J. & Oncken, O. 2016. Zagros blueschists: Episodic underplating and long-lived cooling of a subduction zone. Earth and Planetary Science Letters. 443, 48-58.

  • [17] Rubatto, D. & Angiboust, S., 2015. Oxygen isotope record of fluid metasomatism during subduction: a P-T-time-fluid path for the Monviso eclogites (Italy). Contributions to Mineralogy and Petrology, 170(5).

  • [16] Collins, N., Bebout G.., Angiboust S., Agard P., Scambelluri M., Crispini L & John, T. 2015. Subduction Zone metamorphic pathway for deep carbon recycling: II. Evidence from HP/UHP Metabasaltic rocks and Ophicarbonates . Contributions to Mineralogy and Petrology, 412, 132–150.

  • [15] Angiboust, S., Kirsch J., Oncken, O., Glodny, J., Monié, P. & Rybacki., E,. 2015. Probing the transition between seismically coupled and decoupled segments along an ancient subduction interface. Geochemistry Geophysics Geosystems, 16 (6), 1905-1922.

  • [14] Angiboust, S., Glodny, J., Oncken, O. & Chopin, C., 2014b. In search of transient subduction interfaces in the Dent Blanche-Sesia Tectonic System. Lithos, 205, 298-321.

  • [13] Cook-Collars, J., Bebout, G.E., Collins, N.C., Angiboust, S. & Agard, 2014. Subduction zone metamorphic pathway for deep carbon cycling: I. Evidence from HP/UHP metasedimentary rocks, Italian Alps. Contributions to Mineralogy and Petrology, 386, 31-48.

  • [12] Angiboust, S., Pettke, T., De  Hoog, CJ., Caron, B. & Oncken, O., 2014a. Channelized fluid flow and Eclogite-facies Metasomatism along the Subduction shear zone. Journal of Petrology, 55(5), 883- 916.

  • [11] Moreno, M., Haberland, C., Oncken, O., Rietbrock, A., Angiboust, S. & Heidbach, O., 2014. Locking of the Chile Subduction Zone Controlled by Fluid Pressure before the 2010 Earthquake. Nature Geosciences 7(4), 292-296, doi:10.1038/ngeo2102.

  • [10] Sippl C., Schurr B., Tympel J., Angiboust S., Mechie J., Yuan X., Schneider F.M., Sobolev S.V., Ratschbacher L., Haberland C. and the  TIPAGE-Team, 2013. Active subduction of continental crust beneath the Pamir  imaged with local earthquake tomography. Earth and Planetary Science Letters, 384, 165-177.

  • [9] Castelli, D., Compagnoni, R., Lombardo, B., Angiboust S., Balestro G., Ferrando S., Groppo C. and Rolfo, F., 2013. The Monviso meta-ophiolite complex: HP metamorphism of oceanic crust and interactions with ultramafics. Field guide of the 10th International Eclogite Conference (Courmayeur, September 2013). Periodico del Servicio Geologico d’Italia, 6, n°1-3, 73pp, doi: 10.3301/GFT.2014.03. 

  • [8] Angiboust S., Agard, P., De Hoog, CJ., Omrani, J. & Plunder, A., 2013. Insights on deep, accretionary subduction processes  from the Sistan ophiolitic « mélange » (Eastern Iran). Lithos, 156, 139-158.

  • [7] Angiboust S., Wolf, S., Burov, E., Agard, P. & Yamato, P., 2012d. Effect of Fluid Circulation on Subduction Interface Tectonic Processes: Insights from Thermo-mechanical Numerical Modelling. Earth and Planetary Science Letters, 358, 238-248.

  • [6] Angiboust S., Agard, P., Yamato, P. & Raimbourg, H., 2012c. Eclogite breccias in a subducted ophiolite: a record of intermediate-depth earthquakes? Geology, 40, 707-710.

  • [5] Angiboust S., Fayek, M.,  Power, I., Camacho, A., Calas, G. & Southam, G., 2012b. Structural and  biological control of the cenozoic epithermal uranium concentrations  from the Sierra Peña Blanca, Mexico. Mineralium deposita, 47(8), 859-874.

  • [4] Angiboust S., Langdon R., Agard, P., Waters D. & Chopin C., 2012a.  Eclogitization of the Monviso ophiolite (W. Alps) and implications on  subduction dynamics, Journal of Metamorphic Geology, 30, 37-61. 

  • [3] Angiboust S., Agard, P., Raimbourg, H., Yamato, P. & Huet, B., 2011. Subduction interface processes recorded by eclogite-facies shear zones, Lithos, 127, 222-238.

  • [2] Angiboust S. & Agard P., 2010. Initial water budget: the key to detaching large  volumes of eclogitized oceanic crust along the subduction channel? Lithos, 120, 453-474.

  • [1] Angiboust, S., Agard, P., Jolivet, L., & Beyssac, O., 2009. 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, 21, 171-180.

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