THE LEZ VALLEY TRAVERTINES (MONTPELLIER, SOUTH OF FRANCE) - DATINGS TH-230 U-234 AND PLEISTOCENE ENVIRONMENTS/

Citation
P. Ambert et al., THE LEZ VALLEY TRAVERTINES (MONTPELLIER, SOUTH OF FRANCE) - DATINGS TH-230 U-234 AND PLEISTOCENE ENVIRONMENTS/, Comptes rendus de l'Academie des sciences. Serie II. Sciences de la terre et des planetes, 321(8), 1995, pp. 667-674
Citations number
17
Categorie Soggetti
Multidisciplinary Sciences
ISSN journal
12518050
Volume
321
Issue
8
Year of publication
1995
Pages
667 - 674
Database
ISI
SICI code
1251-8050(1995)321:8<667:TLVT(S>2.0.ZU;2-H
Abstract
Studied since the XIXth century, the Let travertines (Montpellier) hav e not up to now been mapped in any detail. This multidisciplinary stud y with Th-230/U-234 isotopic data shows that the Castelnau-le-Lez trav ertines are diachronic. There are three great phases of travertine dep osits which allowed gouging by the Let during the Upper Pleistocene.