Skip to Main Content

Abstract

The wells at North Haynesville produce oil and gas from oolitic lime grainstones marking the top of the Jurassic Smackover Formation in northern Claiborne Parish, Louisiana. These grainstones are the terminal high energy phase of a regressive sequence deposited on a carbonate ramp which developed across the northern margin of the North Louisiana Salt Dome Basin.

Figures & Tables

Contents

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