Sedimentary responses to forced regressions

An increasing number of studies in recent years have demonstrated that significant progradation of shallow marine systems occurs under conditions of base-level fall. These new data are forcing many sedimentary geologists to critically re-evaluate many aspects of sequence stratigraphy relating to ero...

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Autore principale: Hunt, D.
Altri autori: Gawthorpe, Robert L. (Direttore editoriale)
Natura: Livre numérique
Lingua:Anglais
Pubblicazione: London : Geological society of London [20..].
[London] : Lyell Collection [200.].
Serie:Geological Society, London, special publications 172
Soggetti:
Accesso online:Accès sur la plateforme de l'éditeur
Accès sur la plateforme ISTEX
Accès Université d'Orléans
Accès INSA CVL
Nota: Date de diffusion estimée d'après les informations de la plateforme
Geological Society of London Special Publications GSL e-books (Licence nationale)
Geological Society of London Special Publications GSL e-books (Licence nationale)
Autres localisations: Voir dans le Sudoc
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520 |a An increasing number of studies in recent years have demonstrated that significant progradation of shallow marine systems occurs under conditions of base-level fall. These new data are forcing many sedimentary geologists to critically re-evaluate many aspects of sequence stratigraphy relating to erosion and deposition during base-level (lake- or relative sea-level) fall, and the intrinsic link made between stratal geometries and base-level change. For the first time, this volume brings together a collection of articles that focus solely on forced regressions, providing a more complete picture of the development, formation, variability and preservation of the surfaces and deposits generated during base-level fall. The results of the studies published here will be of interest to all geologists attempting to understand the relationship between changes in base-level and stratigraphy, and to all who use sequence stratigraphy as a method of stratigraphic correlation and interpretation at outcrop and in the subsurface. 
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