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The AAPG/Datapages Combined Publications Database

AAPG Bulletin

Abstract


Volume: 68 (1984)

Issue: 4. (April)

First Page: 481

Last Page: 481

Title: Interactive Geologic Previous HitModelingNext Hit: ABSTRACT

Author(s): J. D. Glaeser, Stephen A. Krajewski, Ron Budros

Abstract:

Improved success in finding hydrocarbons and minerals depends on developing geologic models from Previous HitseismicNext Hit, gravity, and magnetic data that most closely approximate real-world settings. Although data processing remains the chore of mainframe and minicomputers, interpretations and Previous HitmodelingNext Hit of geologic and geophysical information now are best accomplished on personal computers because these computers afford the explorationist maximum freedom to shape and fine tune geophysical evaluations. Three case histories use the GEOSIM geophysical Previous HitmodelingNext Hit systems to delineate exploration targets.

The first example is Silurian Niagaran reef trends in the Michigan basin. Here, differences in Previous HitseismicNext Hit reef anomalies result from variations in carbonate-evaporite stratigraphy encasing the reefs, reef geometry, and reef reservoir parameters. These variations which influence real Previous HitseismicNext Hit-response differences can be successfully matched using appropriate geologic models in generating synthetic Previous HitseismicNext Hit reef anomalies.

The second example applies gravity and magnetic data to Previous HitseismicNext Hit Previous HitmodelingNext Hit of a Wyoming coal field. Detailed Previous HitseismicNext Hit stratigraphy helps locate those portions of the field having multiple seams, although it does not resolve individual economic zones. Gravity data do identify pinchout margins of multiseam zones and pinchouts between principal coals. Magnetic data are then used to delineate the burn (clinker) margin.

Previous HitSeismicNext Hit Previous HitmodelingNext Hit of subtle stratigraphic traps is the broader area of exploration interest contained in the first 2 examples. In the third, successfully modeled and tested examples of lateral changes in deltaic facies and of faulted, unconformity-bounded continent-margin sequences are shown to be successful guides to reinterpretation of Previous HitseismicTop data.

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Copyright 1997 American Association of Petroleum Geologists