Relevant bibliographies by topics / Liguro-Piemont

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  1. Journal articles
  2. Dissertations / Theses

Academic literature on the topic 'Liguro-Piemont'

Author: Grafiati
Published: 25 May 2024
Last updated: 31 July 2025

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Journal articles on the topic "Liguro-Piemont"

1

Herviou, Clément, Philippe Agard, Alexis Plunder, et al. "Subducted fragments of the Liguro-Piemont ocean, Western Alps: Spatial correlations and offscraping mechanisms during subduction." Tectonophysics 827 (March 2022): 229267. http://dx.doi.org/10.1016/j.tecto.2022.229267.

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2

Mendes, Kevin, Philippe Agard, Alexis Plunder, and Clément Herviou. "Lithospheric-scale dynamics during continental subduction: Evidence from a frozen-in plate interface." Geology, October 4, 2023. http://dx.doi.org/10.1130/g51480.1.

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Continental subduction and collision are not merely follow-ups of oceanic subduction but mark the transition from lithospheric-scale deformation localized along the subduction interface to crustal-scale deformation distributed across the orogen. In order to unravel the processes typifying the dynamic changes from oceanic subduction to collision, we have characterized the pressure-temperature (P-T) and spatio-temporal evolution of rocks on each side of the tectonic contact (Briançonnais−Liguro-Piemont [Br-LP] contact) separating the subducted oceanic remnants from the subducted continental frag
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3

Herviou, Clément, Philippe Agard, Anne Verlaguet, et al. "Fractal Distribution of Subduction‐Related Crack‐Seal Veins (Schistes Lustrés, W. Alps): Implications for Fluid Flow and Rupture Processes at the Downdip End of the Seismogenic Zone." Journal of Geophysical Research: Solid Earth 128, no. 10 (2023). http://dx.doi.org/10.1029/2022jb026317.

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AbstractIn the Western Alps, oceanic lithosphere fragments recovered from subduction are exposed continuously across the Liguro‐Piemont domain. In this nappe‐stack, the Schistes Lustrés metasediments are volumetrically dominant and contain large amounts of high‐pressure lawsonite‐ and Fe‐Mg carpholite‐bearing veins. These veins formed close to peak burial conditions at 30–60 km depth where deep slow slips and tremors occur. In the 12 studied outcrops, vein thickness distribution fit power laws while vein spacings and clustering show significant deviations from power laws, interpreted as the re
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4

Maffeis, A., A. Petroccia, S. Nerone, et al. "Filling the gap in the UHP metamorphic record of the Liguro-Piemont lower unit: Insights on fluid-mediated formation of atoll garnets." Lithos, February 2025, 107981. https://doi.org/10.1016/j.lithos.2025.107981.

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5

Herviou, Clément, Guillaume Bonnet, Samuel Angiboust, Aitor Cambeses, and Tom Raimondo. "Petrochronology of High‐Pressure Veins Reveals the Evolution of Fluid Sources in Subducted Oceanic Crust (Rocciavrè Eclogites, W. Alps)." Journal of Metamorphic Geology, January 16, 2025. https://doi.org/10.1111/jmg.12806.

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ABSTRACTThe Rocciavrè massif is a large eclogitized ophiolitic fragment exposed in the Western Alps (Piemonte, Italy) exhibiting an almost complete sequence of the subducted Liguro‐Piemont lithosphere. Raman spectroscopy on carbonaceous material in metasediments from Rocciavrè and the juxtaposed Orsiera massif indicates maximum temperatures in the range ~510°C–550°C, whereas thermodynamic modelling in mafic lithologies reveals peak burial metamorphic conditions of 550°C–590°C/2.2–3.0 GPa for both units, suggesting the absence of a metamorphic gap between them. Late Jurassic (ca. 151–158 Ma) zi
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Dissertations / Theses on the topic "Liguro-Piemont"

1

Herviou, Clément. "Circulations de fluides et mécanismes de déformation dans les Schistes Lustrés Liguro-Piémontais : implications pour le fonctionnement des zones de subduction." Electronic Thesis or Diss., Sorbonne université, 2022. https://accesdistant.sorbonne-universite.fr/login?url=https://theses-intra.sorbonne-universite.fr/2022SORUS142.pdf.

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Ce travail vise à caractériser les fluides circulant dans une zone de subduction fossile, entre ~30 et 80 km de profondeur dans le cas d'étude retenu, celui du domaine Liguro-Piémontais alpin. L'étude des conditions métamorphiques enregistrées par les écailles tectoniques exhumées y révèle une distribution trimodale d’unités. Les fluides piégés, témoins de la circulation en contexte de subduction, ont été étudiés dans les veines de haute pression, notamment dans les sédiments des unités supérieures et médianes. La composition des inclusions fluides, ainsi que l’étude statistique de la distribu
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