Skip to Main Content
Book Chapter

Hydrocarbon-induced diagenetic aureole at Cement-Chickasha Anticline, Oklahoma

By
Zuhair Al-Shaieb
Zuhair Al-Shaieb
School of Geology, Oklahoma State University, Stillwater, Oklahoma 74078
Search for other works by this author on:
Published:
January 01, 1988

Abstract

The Cement-Chickasha Anticline includes parts of Caddo and Grady counties in southwestern Oklahoma (Fig. 1). The structure is elongated and trends in a northwesterly direction. The town of Cement is located in the central part of the structure. Three major highways intersect the site. The H. E. Bailey Turnpike extends diagonally across the southeastern portion of the site, while U.S. 277/Oklahoma 19 trends east–west through the southern half of the site and connects the towns of Cement and Cyril. Oklahoma 8 trends north-south through the western portion of the site and terminates at the town of Cyril.

You do not currently have access to this article.
Don't already have an account? Register

Figures & Tables

Contents

DNAG, Centennial Field Guides

South-Central Section of the Geological Society of America

O. T. Hayward
O. T. Hayward
Geology Department, Baylor University, Waco, Texas 76798
Search for other works by this author on:
Geological Society of America
Volume
4
ISBN electronic:
9780813754109
Publication date:
January 01, 1988

GeoRef

References

Related

A comprehensive resource of eBooks for researchers in the Earth Sciences

Close Modal
This Feature Is Available To Subscribers Only

Sign In or Create an Account

Close Modal
Close Modal