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(Article of periodic en Anglais - 1993)

Document title

Cainozoic heritage in the modern landscape near Bungonia, southern New South Wales

Authors(s) and Affiliation(s)

WRAY R.A. ; YOUNG R.W. ; PRICE D.M. ;

Abstract

The regional topography of much of the New South Wales Southern Highlands was long attributed to Quaternary erosion, but it has been recently demonstrated that the region was, in fact, well developed by the Eocene. Stratigraphic techniques, U/Th, TL and [14]C dating aid reconstruction of much of Inverary Park. Major changes in sediment type and source have long been common, but late Quaternary changes do not correlate well with similar observations elsewhere, suggesting that changes in hydrologic regime, notably climate change, are not necessarily responsible for changes in the stratigraphic record

Source

Article of periodic

published at : Australian Geographer / ISSN 0004-9182

Editor : Geographical Society of New South Wales, Sydney - AUSTRALIE (1928)

Millesime : 1993, vol. 24, no1 [pp. 45-61]

Bibliographic references : 72 réf.

Collation : Illustration ;

Language

Anglais

INIST-CNRS, Cote INIST : 3519

Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 1994.
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