Published 1995 | Version v1
Book

A 10Be profile in mid-pleistocene sediments of the Wanganui Basin, New Zealand

  • 1. Institute of Geological and Nuclear Sciences Limited, Nuclear Sciences, Lower Hutt (New Zealand)

Description

A 10Be study of marine sediments from the Wanganui Basin (Castlecliff Section) has yielded some interesting, though not immediately explainable results. A 5-6 fold increase in 10Be has been identified immediately above the Brunhes-Matuyama paleomagnetic reversal within the sedimentary sequence, ca. 780 ka. The increase in 10Be cannot be attributed entirely to the paleomagnetic reversal, and probably reflects the major global climatic change at that time resulting in an influx of 10Be during post-glacial melting. (authors) 30 refs., 4 figs., 3 tabs

Availability note (English)

Available form the Institute of Geological and Nuclear Sciences, PO Box 31-312, Lower Hutt, New Zealand.

Additional details

Publishing Information

Publisher
Institute of Geological and Nuclear Sciences.
Imprint Place
Lower Hutt (New Zealand)
ISBN
0-478-08850-7
Imprint Pagination
15 p.
Journal Issue
no.95/13
Series
Institute of Geological and Nuclear Sciences science report.
ISSN
1171-9184