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Abstract


 
Chapter from: SG 42:  Applications of 3-D Seismic Data to Exploration and Production

Edited by: 
Paul Weimer and Thomas L. David

Authors:
Goeffrey A. Dorn, Kenneth M. Tubman, Dennis Cooke, and Rob O'Connor

Published 1996 as part of Studies in Geology 42
Copyright © 1996 The American Association of Petroleum Geologists.  All Rights Reserved.
 

*Editorial Note: Page numbers in this digital version (HTML and PDF) do not correspond to those of the hardcopy.
Otherwise, the two are the same.
 
 

CHAPTER 11

Chapter 11: Geophysical Reservoir Characterization of Pickerill Field, North Sea, Using 3-D Seismic and Well Data

Geoffrey A. Dorn*, Kenneth M. Tubman*, Dennis CookeÝ, and Rob O'Connor§

 

Dorn, G., K. Tubman, D. Cooke, and R. O'Connor, Geophysical Reservoir Characterization of Pickerill Field, North Sea, Using 3-D Seismic and Well Data, in P. Weimer and T. L. Davis, eds., AAPG Studies in Geology No. 42 and SEG Geophysical Development Series No. 5 AAPG/SEG, Tulsa, p. 107-122.
ABSTRACT

Pickerill Field is a relatively thin, highly faulted gas reservoir in the southern gas basin of the North Sea. The 100- to 250-ft (30-to 76-m) thick, Permian Rotliegend reservoir consists primarily of thin dune and interdune deposits overlying generally poorer-quality fluvial sands. There is a rapid lateral variation in reservoir quality due to facies changes and compartmentalization due to diagenesis associated with faults.

A combination of petrophysics and geophysics was used to develop seismic criteria that could be used to optimize the location of development wells. An analysis of horizon attributes from the 3-D seismic survey produced a detailed reservoir fault map. Analysis of log data, seismic modeling, and horizon attributes produced an estimated reservoir porosity map. These have been used to help optimize the position of development wells in the field.

A detailed interpretation was made of several horizons in the 3-D seismic survey, including the Top Rotliegend (top reservoir) reflection. A set of seismic horizon attributes, based on horizon structure and reflection amplitude, were generated at the Top Rotliegend. Reservoir faults with throws as small as 15 ft (5 m) were interpreted and mapped. Since many faults were sealed by diagenesis subsequent to faulting, these results have helped identify potential compartmentalization and have allowed development wells to be positioned away from these potential barriers to flow.

Synthetic seismic modeling using log data from exploration wells indicated a linear relationship between reservoir reflection amplitude and average reservoir porosity. Log-based wavelet extraction was used to correct phase errors in the seismic data. Phase-corrected reflection amplitude from the Top Rotliegend reflection was correlated with porosity at exploration wells. The resulting empirical amplitude-porosity relationship has been used to successfully predict gross reservoir porosity in several wells drilled since the work was concluded.

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