About This Item

Share This Item

The AAPG/Datapages Combined Publications Database

AAPG Special Volumes

Abstract

J. W. Robinson and K. W. Shanley, 2004, Jonah Field: Case Study of a Tight-Gas Fluvial Reservoir , AAPG Studies in Geology 52 and Rocky Mountain Association of Geologists 2004 Guidebook.

Copyright copy2004. The American Association of Petroleum Geologists. All rights reserved.

The Origin of Jonah Field, Northern Green River Basin, Wyoming

Robert M. Cluff, Suzanne G. Cluff

The Discovery Group Inc., Denver, Colorado, U.S.A.

ACKNOWLEDGMENTS

The authors acknowledge the contributions of numerous colleagues and clients we have worked with over the years on the Jonah problem, many of whom contributed substantially to the development of the ideas presented in this chapter. These include Alan Byrnes of the Kansas Geological Survey, and John Webb of The Discovery Group, with whom we first started working on the petrophysical aspects of Jonah back in 1994; Dennis Storhaug and Denise Delozier, both formerly with Snyder Oil Company; Kent Bowker and Deane Foss, both formerly with Chevron U.S.A.; Dean DuBois, EnCana U.S.A.; Jim Folcik, EOG Resources; and Phil Winner, formerly with HS Resources. We especially thank Keith Shanley and John Robinson for uncounted hours of discussion on the dilemma of the origin of the pressure conditions around Jonah and for their support in the preparation of this chapter.

ABSTRACT

Prolific production at Jonah field and many other fields in the Green River basin is dependent on the presence of overpressure. In the Gulf Coast and other areas, plots of shale resistivity and shale sonic transit time versus depth have been used to identify overpressured zones. The same technique has been proposed to map overpressure compartments and their boundaries in the Rocky Mountain region using well logs or, alternatively, interval velocities determined from seismic data. At Jonah field, the top of the overpressure (determined by continuous gas flaring during drilling) correlates within a few hundred feet to a drop in shale resistivity and increase in shale transit time. However, studies of nearby wildcat wells and detailed cross sections through both overpressured and normally pressured wells show that the log anomalies extend significantly beyond the overpressured area. Velocity and resistivity changes in the area around Jonah tend to follow a stratigraphic boundary near the base of the Tertiary Fort Union Formation instead of tracking the top of the overpressured volume.

Early studies of Jonah field considered the hydrocarbons in the field to be derived from vertical migration of gas from regional overpressure conditions 2000–3000 ft (610–915 m) deeper. The upward migration was presumed to be controlled by the presence of extensive microfractures that form a leakage chimney between large sealing faults. This study suggests that the log anomaly both within and surrounding Jonah provides an alternative interpretation. Until the middle Tertiary, overpressure conditions extended up to the base of the Fort Union and resulted in undercompaction of Cretaceous shales, as reflected by resistivity and velocity anomalies. Late Tertiary relative uplift initiated slow leakage of the overpressure conditions wherever the system was not tightly sealed. As a result, the top of the overpressure has been dropping with time over most of the northern Green River basin. The sonic and resistivity anomalies are irreversible, and the logs reveal the signature of the former overpressured and undercompacted conditions.

Based on this new model, Jonah field represents a high remnant of the former regional top of overpressure instead of a leakage chimney from a deeper overpressured generation cell. If this model is correct, exploration methods should focus on the seal conditions that prevent leakage instead of fracture models that promote leakage.

Pay-Per-View Purchase Options

The article is available through a document delivery service. Explain these Purchase Options.

Watermarked PDF Document: $14
Open PDF Document: $24