FN Archimer Export Format
PT J
TI Taux de sédimentation dans l'étang de Thau à partir des données géochronologiques, géochimiques et des repères stratigraphiques
OT Sedimentation rate in the Thau basin (France) according to geochronological, geochemical and stratigraphical data.
BT 
AF MONNA, F
   LANCELOT, J
   BERNAT, M
   MERCADIER, H
AS 1:;2:;3:;4:;
FF 1:;2:;3:;4:;
C1 UNIV MONTPELLIER 2,CNRS,URA 5567,LAB GEOCHIM ISOTOP,F-34095 MONTPELLIER 05,FRANCE
   UNIV NICE,CNRS,URA 132,LAB GEOCHIM ISOTOP,F-06000 NICE,FRANCE
C2 UNIV MONTPELLIER 2,CNRS,URA 5567,LAB GEOCHIM ISOTOP,F-34095 MONTPELLIER 05,FRANCE
   UNIV NICE,CNRS,URA 132,LAB GEOCHIM ISOTOP,F-06000 NICE,FRANCE
IF 0.662
TC 10
UR https://archimer.ifremer.fr/doc/00093/20422/18089.pdf
LA French
DT Article
AB Geochronological data (Pb-210) Obtained on four sediment cores, coupled with geochemical analysis, X-ray radiography, meteorological data and stratigraphical observations, made it possible to provide a recent and coherent sedimentary history of the Thau basin (Herault, France). Cluster analysis of major elements isolates some horizons presenting a strong terrigenous signature, which are also identified by X-ray. These strata, characterized by high Al, Fe, Ti and K contents, are the consequence of the exceptional flood which occurred in September 1875. This event serves to calibrate the radiochronological data, which are limited at 100 years. Cores located close to the continental and fluviatile inputs accurately record the flood horizon. Measured sedimentation rates range between 0.09 and 0.18 g.cm(-2).yr(-1) and are in general agreement with the knowledge concerning the dynamic of the basin.
PY 1997
SO Oceanolica Acta
SN 0399-1784
PU Gauthier-Villars
VL 20
IS 4
UT A1997XU31400005
BP 627
EP 638
ID 20422
ER

EF