Serveur d'exploration sur le chêne en Belgique (avant curation)

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Géométrie et âge des alluvions du lit majeur de la Loire moyenne, exemple du val d'Avaray (Loir-et-Cher, France)

Identifieur interne : 000F82 ( Main/Exploration ); précédent : 000F81; suivant : 000F83

Géométrie et âge des alluvions du lit majeur de la Loire moyenne, exemple du val d'Avaray (Loir-et-Cher, France)

Auteurs : Manuel Garcin [France] ; Denis Giot [France] ; Geneviève Farjanel [France] ; Jean-Christophe Gourry [France] ; Wolfram Kloppmann [France] ; Philippe Negrel [France]

Source :

RBID : ISTEX:9D98FE65A7001314E00384C9A11AF59A89FBEBF1

Descripteurs français

English descriptors

Abstract

Abstract: Incision and infilling of the flood plain of the Loire river, in the Val d'Avaray area, is polyphased during Tardiglacial and Holocene. Five main alluvial units are developed and result from successive meandering-like phases of erosion and sandy infilling. Clayey channel fillings sometimes associated with peat have been identified within the sandy units. The first investigated channel was active from Tardiglacial (11.4 ka BP, Allerød) to Boreal, the second one from 8.4 ka BP (Boreal) to 2.3 ka BP (Subatlantic) with an average sedimentation rate of 0.5 mm·yr−1. A third one was active from 3.2 ka BP (Subboreal) and during a great part of the Subatlantic; the average rate of sedimentation is evaluated at 1.3 mm·yr−1.

Url:
DOI: 10.1016/S1251-8050(00)80064-6


Affiliations:


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