About This Item

Share This Item

The AAPG/Datapages Combined Publications Database

AAPG Special Volumes

Abstract


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

Edited by: 
Paul Weimer and Thomas L. David

Authors:
Kathleen O. Horkowitz and David R. Davis


 


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 4

Chapter 4: Seismic Delineation of Thin Sandstone Reservoirs in a Shale-Rich Sequence Using Previous HitInstantaneousNext Hit Frequency and Reflection Amplitude Previous HitAttributesNext Hit from 3-D Data, Texas Gulf Coast

Kathleen O. Horkowitz* and David R. Davis**

Horkowitz, K. O., and D. R. Davis, Seismic delineation of thin sandstone reservoirs in a shale-rich sequence using Previous HitinstantaneousNext Hit frequency and reflection amplitude Previous HitattributesNext Hit from 3-D data, Texas Gulf Coast, in P. Weimer and T. L. Davis, eds., AAPG Studies in Geology No. 42 and SEG Geophysical Developments Series No. 5, AAPG/SEG, Tulsa, p. 35-44.
ABSTRACT


A combination of seismic trace Previous HitattributesNext Hit including Previous HitinstantaneousNext Hit frequency and reflection amplitude was successfully used to seismically delineate gas-prone reservoir facies consisting of thin, discontinuous sandstone reservoirs in a shale-rich stratigraphic sequence. This type of reservoir section poses special problems for seismic interpretation due to a high degree of lateral and vertical variation in the ratio of net sandstone to gross interval thickness. Individual sandstone reservoirs are also below the limit of seismic bed resolution, further complicating the evaluation.

Previous HitInstantaneousNext Hit frequency maps were used directly to map the areal distribution of reservoir-prone intervals. The addition of calibrated average amplitude maps provided the ability to discriminate between homogenous shale-rich sections and relatively homogenous sandstone-rich sections characterized by amalgamated siltstones and sandstones. The lithofacies prediction model developed using this integrated geological, petrophysical, and seismic interpretation technique was confirmed by the results of two new wells which penetrated the target interval described in this study. Previous HitInstantaneousTop frequency maps with overlays of amplitude and time structure contours successfully identified stratigraphic intervals favorable for gas accumulation and trapping.

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