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(Article of periodic en Anglais - 1996)

Document title

Origin of the Whewellite-rich rock crust in the Lower Pecos Region of Southwest Texas and its significance to paleoclimate reconstructions

Authors(s) and Affiliation(s)

RUSS J. (1) ; PALMA R.L. ; LOYD D.H. ; BOUTTON T.W. ; COY M.A. ;
(1) Dept. of Chemistry, Newberry College, Newberry, South Carolina, ETATS-UNIS

Abstract

This study focuses on the rock crust that occurs in sheltered areas in the limestone cliffs along the lower Pecos River, the Rio Grande near the Pecos confluence, and canyon tributaries of the two rivers. A preliminary paleoclimate reconstruction based on 14 AMS C 14 dates indicates the Lower Pecos experienced dry to wet climate fluctuations during the late Holocene. This reconstruction generally agrees with other models established for Texas

Source

Article of periodic

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

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

Millesime : 1996, vol. 46, no1 [pp. 27-36]

Bibliographic references : 54 ref.

Collation : Illustration ;

Language

Anglais

INIST-CNRS, Cote INIST : 15739

Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 1996.
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