--> Abstract: Seismic Modeling of Carbonate Outcrops, by J. Stafleu, W. Schlager, E. Campbell, and A-J. Everts; #90990 (1993).
[First Hit]

Datapages, Inc.Print this page

STAFLEU, JAN, WOLFGANG SCHLAGER, EWAN CAMPBELL, and ARNOUT-JAN EVERTS, Vrije Universiteit, Amsterdam, Netherlands

ABSTRACT: Previous HitSeismicNext Hit Modeling of Carbonate Outcrops

Traditionally, Previous HitseismicNext Hit modeling has concentrated on one-dimensional borehole modeling and Previous HittwoNext Hit-Previous HitdimensionalNext Hit forward modeling of basic structural-stratigraphic schemes, which are directly compared with real Previous HitseismicNext Hit Previous HitdataNext Hit. Previous HitTwoNext Hit-Previous HitdimensionalNext Hit Previous HitseismicNext Hit models based on outcrop observations may aid in bridging the gap between the detail of the outcrop and the low resolution of Previous HitseismicNext Hit lines. Examples include the Dolomites (north Italy), the High Atlas (Morocco), the Vercors (southeast France) and the Last Chance Canyon (New Mexico).

The Previous HitseismicNext Hit models generally are constructed using the following procedure: (1) construction of a detailed lithological model based on direct outcrop observations; (2) division of the lithological model into lithostratigraphic units, using master bedding planes and important facies transitions as boundaries; (3) assignment of petrophysical properties to these lithostratigraphic units; (4) computation of time sections of reflectivity, using different modeling techniques; and (5) convolution with source wavelets of different frequencies.

The lithological detail modeled in the case studies lead to some striking results, particularly the discovery of pseudo-unconformities. Pseudo-unconformities are unconformities in seismics, but correspond to rapid changes of dip and facies in outcrop. None of the outcrop geometries studied were correctly portrayed seismically at 25 Hz frequency. However, in some instances the true relationship would emerge gradually at frequencies of 50 to 100 Hz.

These results demonstrate that detailed, outcrop-derived/Previous HitseismicNext Hit models can reveal what stratigraphic relationships and features are likely to be resolved under ideal or less ideal conditions, and what pitfalls may befall the interpreter of real Previous HitseismicNext Hit Previous HitdataTop.

AAPG Search and Discovery Article #90990©1993 AAPG International Conference and Exhibition, The Hague, Netherlands, October 17-20, 1993.