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The AAPG/Datapages Combined Publications Database

AAPG Bulletin

Abstract


Volume: 68 (1984)

Issue: 4. (April)

First Page: 525

Last Page: 525

Title: Previous Hit3-DNext Hit Previous HitSeismicNext Hit Interactive Interpretation of Complex Stratigraphic Environments: An Example From Grayson County, Texas: ABSTRACT

Author(s): A. C. Schlosser, D. G. Jovanovich, R. C. Jones, J. H. Caldwell

Abstract:

Interactive interpretation of Previous Hit3-DNext Hit Previous HitseismicNext Hit Previous HitdataNext Hit is now an effective tool for mapping complex stratigraphic targets on land. Slicing a Previous Hit3-DNext Hit Previous HitseismicNext Hit Previous HitcubeNext Hit through a single reflector provides an insight into complex stratigraphic environments.

A case study from Grayson County, Texas, is used as an example. Production from the lower Davis sands of the Atokan series was established in the Southmaud area in 1978. Further development of the field led to a success ratio of only 50%. Stratigraphic complexity of the fluvial to deltaic environment made reservoir prediction and placement of offset wells difficult. A 6-mi2 Previous Hit3-DNext Hit survey was shot for the purpose of mapping the sand distribution. Acquisition and processing costs were less than the cost of one dry hole. The producing sands were a difficult Previous HitseismicNext Hit target. Resolution of these sand bodies was in question due to their vertical and horizontal extent as well as their small reflection coefficients.

The interpretation was completed in eighteen hours using Gulf's Interactive Previous HitSeismicNext Hit Interpretation System (ISIS). Only one well was used initially to identify Previous HitseismicNext Hit horizons. Structural mapping was completed using dual polarity, random vertical lines, and isotime slices. Stratigraphic interpretation was done with discrete amplitude coloring to take advantage of Previous HitseismicTop tuning effects. Stratigraphic slices revealed the distribution and thickness of the reservoir sand. Geological features interpreted include a meandering channel with point-bar buildups, a distributary complex, and erosional or nondepositional areas.

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