Skip to Main Content
Book Chapter

Bioclastic Turbidites in the Trenton Limestone: Significance and Criteria for Recognition

By
Charlotte J. Mehrtens
Charlotte J. Mehrtens
University of Vermont Burlington, Vermont
Search for other works by this author on:
Published:
January 01, 1988

Abstract

The Denley Limestone (Trenton Group) in the Mohawk Valley, New York, is composed of bioclastic turbidites associated with slump fold horizons and syndepositional block faults which indicate that the limestones of the Denley Formation are foreland basin/trench slope deposits.

You do not currently have access to this article.

Figures & Tables

Contents

AAPG Studies in Geology

The Trenton Group (Upper Ordovician Series) of Eastern North America: Deposition, Diagenesis, and Petroleum

Brain D. Keith
Brain D. Keith
Search for other works by this author on:
American Association of Petroleum Geologists
Volume
29
ISBN electronic:
9781629811352
Publication date:
January 01, 1988

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