EVOLUTION OF THE SEDIMENTARY FLUXES DURIN G THE POSTGLACIAL PERIOD - RECORD IN THE LACUSTRINE INFILLING AT CHAILLEXON (DOUBS, FRANCE)

Authors
CAMPY M BICHET V DIGIOVANNI C RICHARD H DURAND A
Citation
M. Campy et al., EVOLUTION OF THE SEDIMENTARY FLUXES DURIN G THE POSTGLACIAL PERIOD - RECORD IN THE LACUSTRINE INFILLING AT CHAILLEXON (DOUBS, FRANCE), Comptes rendus de l'Academie des sciences. Serie 2, Mecanique, physique, chimie, sciences de l'univers, sciences de la terre, 319(1), 1994, pp. 103-109
Citations number
8
Categorie Soggetti
Multidisciplinary Sciences
Journal title
Comptes rendus de l'Academie des sciences. Serie 2, Mecanique, physique, chimie, sciences de l'univers, sciences de la terre → ACNP
ISSN journal
07644450
Volume
319
Issue
1
Year of publication
1994
Part
2
Pages
103 - 109
Database
ISI
SICI code
0764-4450(1994)319:1<103:EOTSFD>2.0.ZU;2-Y
Abstract
A landslide dammed the upper Doubs valley around 12 ka BP forming a la ke that has now been filled to 9/10 of its original volume. Sediments from the enclosing basin reveal three phases: - 12 to 9 ka BP, exclusi vely detrital material from mechanical erosion; - 9 to 6 ka BP, materi al dominated by elements in solution, from chemical erosion; - 6 ka BP to present day, a moderate upturn in detrital sedimentation.