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2012-08-18

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Si us plau utilitzeu sempre aquest identificador per citar o enllaçar aquest document: https://hdl.handle.net/2445/34456

Microtextural investigation (SEM and TEM study) of phyllosilicates in a major thrust fault zone (Monte Perdido, southern Pyrenees): impact on fault reactivation

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Recurs relacionat

http://dx.doi.org/10.1007/s00015-012-0098-0

Resum

Thrusting fault zone in foreland basins are characterized by highly foliated zones generally enriched in phyllosilicates which can play a major role on the mechanical behaviour of the fault. In this context, investigations of synkinematic clay minerals permit to determine the origin of the fluid from which they precipitated as well as the mechanisms of deformation. Our study is focused on clay mineral assemblages (illite and chlorite) in a major thrust fault located in the Monte Perdido massif (southern Pyrenees), a shallow thrust that affects upper cretaceouspaleocene platform carbonates and lower Eocene marls and turbidites.

Matèries

Silicats, Pirineu aragonès (Aragó)

Matèries (anglès)

Silicates, Aragon Pyrenees (Aragon)

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Col·leccions

Articles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada)

Citació

BUATIER, Martine, LACROIX, Brice, LABAUME, Pierre, MOUTARLIER, Virginie, CHARPENTIER, Delphine, SIZUN, Jean pierre, TRAVÉ I HERRERO, Anna. Microtextural investigation (SEM and TEM study) of phyllosilicates in a major thrust fault zone (Monte Perdido, southern Pyrenees): impact on fault reactivation. _Swiss Journal Of Geosciences_. 2012. Vol. 105, núm. 313-324. [consulta: 24 de gener de 2026]. ISSN: 1661-8726. [Disponible a: https://hdl.handle.net/2445/34456]

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