Skip to Main Content
Book Chapter

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

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


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.
Don't already have an account? Register

Figures & Tables


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
ISBN electronic:
Publication date:
January 01, 1988




A comprehensive resource of eBooks for researchers in the Earth Sciences

This Feature Is Available To Subscribers Only

Sign In or Create an Account

This PDF is available to Subscribers Only

View Article Abstract & Purchase Options

For full access to this pdf, sign in to an existing account, or purchase an annual subscription.

Subscribe Now