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- W2065471792 abstract "L'analyse combinée des structures tectoniques et des faciès conduit à interpréter le flysch Crétacé supérieur de Saint-Jean-de-Luz comme faisant partie du bassin flexural nord-pyrénéen, actif à partir du Turonien. Cet exemple illustre l'évolution des zones de chevauchement dans le stade d'initiation du raccourcissement en milieu profond et à taux de sédimentation réduit. La formation et la migration des dépocentres sont reliées à la propagation d'un système de chevauchement frontal aveugle. Le flysch est lui-même subdivisé en séquences de dépót. Ces séquences enregistrent les stades de propagation des chevauchements à travers des cortèges de bas niveau relatif, reliés à l'accélération de l'activité tectonique et des cortèges de haut niveau, reliés au ralentissement de cette activité. The integrated analysis of thrust structures and fades allows us to interpret the late Cretaceous flysch basin of Saint-Jean-de-Luz as a North-Pyrenean foreland basin active since Turanian times. This example illustrates the tectono-sedimentary evolution of fold-and-thrust belts in the early stage of shortening in deep marine and starved environments. The formation and the migration of the depocenters are related to the propagation of a blind frontal thrust. The sedimentary infill of the basin is subdivided into numerous depositional sequences, tectonic in origin. They consist of lowstand system tracts related to an increase in tectonic activity, and highstand system tracts related to a decrease in this activity." @default.
- W2065471792 created "2016-06-24" @default.
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- W2065471792 date "1997-08-01" @default.
- W2065471792 modified "2023-09-25" @default.
- W2065471792 title "Évolution tectono-sédimentaire des bassins flexuraux profonds et à taux de sédimentation réduit : exemple du bassin de flysch de Saint-Jean-de-Luz (Pyrénées-Atlantiques, France) au Crétacé supérieur" @default.
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- W2065471792 doi "https://doi.org/10.1016/s1251-8050(97)88299-7" @default.
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