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(Article of periodic en Anglais - 2000)

Document title

Stratigraphic evidence for the uplift of the Tibetan Plateau between 1.1 and 0.9 myr ago

Authors(s) and Affiliation(s)

SUN J. ; LIU T. ;

Abstract

Uplift of the Tibetan Plateau is manifest not only in widespread denudation, but also by an increased deposition rate of sediment, near or far from the exhumed regions. This paper uses the stratigraphic evidence to examine the timing of the Tibetan Plateau uplift during the Pleistocene. The results indicate that the mass accumulation rate (MAR) of eolian dust increased between 1.1 and 0.9 myr ago. They associate this increase in MAR and median grain size with uplift of the Tibetan Plateau and its adjacent regions during this period

Source

Article of periodic

published at : Quaternary research / ISSN 0033-5894 / CODEN QRESAV

Editor : Elsevier, San Diego, CA - ETATS-UNIS (1970)

Millesime : 2000, vol. 54, no3 [pp. 309-320]

Bibliographic references : 54 ref.

Collation : Illustration ;

Language

Anglais

INIST-CNRS, Cote INIST : 15739

Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 2001.
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