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(JerusalemIGU-GERTEC Conference en Anglais - 1998)

Document title

Reconstruction of palaeoenvironmental conditions by investigation of Holocene playa sediments in the Ebro Basin, Spain : preliminary results

published at : Special issue. Geomorphic response of mediterranean and arid areas to climate change

Authors(s) and Affiliation(s)

SCHÜTT B. ;

Abstract

First results of the analysis of the geochemistry and mineralogy of sediments from two endorheic basins within the central Ebro Basin, the Las Plañas de Bujaraloz (west of Zaragoza) and the Desierto de calanda (southwest of Alcañiz) indicate that the climatic conditions governing sedimentation during the Holocene changed from humid and subhumid to the present subarid conditions, but was interrupted by a phase of increased humidity. The varying character of solid bedrock caused different weathering products, which are reflected in the varying geochemical and mineralogical composition of lake deposits

Source

Congrès

IGU-GERTEC Conference, Jerusalem , ISRAEL (13/05/1995)

published at : Geomorphology / ISSN 0169-555X

Editor : Elsevier, Amsterdam - PAYS-BAS (1987)

Millesime : 1998, vol. 23, no 2-4 [pp. 273-283]

Bibliographic references : 29 ref.

Language

Anglais

INIST-CNRS, Cote INIST : 21151

Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 1998.
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