Skip to Main Content
Book Chapter

Isotopic Methods in Quaternary Geology1

By
Vladimir Šibrava
Vladimir Šibrava
Search for other works by this author on:
Published:
January 01, 1978

Abstract

Results achieved in different Quaternary sediments by different methods are discussed, especially with regard to the worldwide correlation of Quaternary sediments. The necessity of a mutual checking of isotopic dating results by other geologic, paleontologic, and geophysical methods is stressed. There is danger of overestimating some methods of absolute dating (in Quaternary geology) which has led in many cases to false stratigraphic conclusions. There is danger especially in conditions of continental sedimentation, where the Quaternary is characterized by the alternation of different genetic and lithologic types of deposits. Isotopic methods must be regarded only as one of the existing methods leading to the establishment of a geochronologic scale, considering the many existing breaks of sedimentations.

You do not currently have access to this article.

Figures & Tables

Contents

AAPG Studies in Geology

Contributions to the Geologic Time Scale

George V. Cohee
George V. Cohee
Search for other works by this author on:
Martin F. Glaessner
Martin F. Glaessner
Search for other works by this author on:
Hollis D. Hedberg
Hollis D. Hedberg
Search for other works by this author on:
American Association of Petroleum Geologists
Volume
6
ISBN electronic:
9781629812007
Publication date:
January 01, 1978

GeoRef

References

Related

Citing Books via

Close Modal
This Feature Is Available To Subscribers Only

Sign In or Create an Account

Close Modal
Close Modal