Interactions climat-eustatisme-tectonique. Les enseignements et perspectives du Crétacé supérieur (Cénomanien-Coniacien)
Identifieur interne : 000E55 ( Main/Exploration ); précédent : 000E54; suivant : 000E56Interactions climat-eustatisme-tectonique. Les enseignements et perspectives du Crétacé supérieur (Cénomanien-Coniacien)
Auteurs : Fabrice Malartre [France] ; Serge Ferry [France] ; Jean-Loup Rubino [France]Source :
- Geodinamica Acta [ 0985-3111 ] ; 1998.
English descriptors
- KwdEn :
Abstract
Abstract: A recent detailed analysis of southeastern France upper Cretaceous series has evidenced that Cenomanian-Turonian and Turonian-Coniacian boundaries are marked by quick and large amplitude relative sea level changes. Comparisons with other sections in different worldwide basins are coincident with the observations pointed out in southeast France. We establish: (1) high-frequency synchronous events in different geodynamic settings, (2) the superposition of various hierarchically eustatic cycles i.e. the superimposition of high-frequency oscillations on a third-order trend. Two possible mechanisms responsible of these observations are emphasized and discussed: glacio-eustasy versus high-frequency tectonics.
Url:
DOI: 10.1016/S0985-3111(99)80016-3
Affiliations:
- France
- Auvergne-Rhône-Alpes, Grand Est, Lorraine (région), Rhône-Alpes, Île-de-France
- Paris La Défense, Vandœuvre-lès-Nancy, Villeurbanne
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Le document en format XML
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Comparisons with other sections in different worldwide basins are coincident with the observations pointed out in southeast France. We establish: (1) high-frequency synchronous events in different geodynamic settings, (2) the superposition of various hierarchically eustatic cycles i.e. the superimposition of high-frequency oscillations on a third-order trend. 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