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- W2019426722 abstract "Normal fault zones affecting the pre-rift limestones in the Corinth Rift comprise breccia corridors separated by slip surfaces, but also numerous stylolites and calcite veins attesting the importance of fluid-driven mass transfer during a(inter)seismic episodes of fault activity. Cathodoluminescence microscopy shows that external (meteoric?) waters circulated in the fault zones, whereas mass transfer in the surrounding rocks implied a closed system with water chemically equilibrated with the host limestone. From these observations, we propose preliminary qualitative models of structural development and fluid flow in active normal fault zones in superficial conditions, with a tendency to concentration of deformation and fluid-flow-related to fault-tip propagation. To cite this article: P. Labaume et al., C. R. Geoscience 336 (2004). Les zones de failles normales affectant les calcaires pré-rift du rift de Corinthe comportent des couloirs bréchiques séparés par des surfaces de glissement, mais aussi de nombreux stylolites et veines de calcite, attestant l'importance des transferts de matière dans les fluides pendant les épisodes a(inter)sismiques de l'activité des failles. La microscopie en cathodoluminescence montre que des eaux externes (météoriques ?) ont circulé dans les zones de failles, alors que le transfert de matière dans les roches adjacentes correspondait à un système fermé, avec des eaux chimiquement équilibrées avec le calcaire hôte. À partir de ces observations, nous proposons un modèle qualitatif préliminaire de développement structural et de circulation de fluides dans des zones de failles normales actives en conditions superficielles, avec une tendance à la concentration de la déformation et de l'écoulement, en relation avec la propagation de l'extrémité de la faille. Pour citer cet article : P. Labaume et al., C. R. Geoscience 336 (2004)." @default.
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- W2019426722 date "2004-03-01" @default.
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- W2019426722 title "Deformation mechanisms and fluid-driven mass transfers in the recent fault zones of the Corinth Rift (Greece)" @default.
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- W2019426722 doi "https://doi.org/10.1016/j.crte.2003.11.010" @default.
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