--> ABSTRACT: Imaging Structural Geology with Dip and Directional Dip, by Aqrawi, Ahmed A.; Boe, Trond Hellem; #90141 (2012)
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Imaging Structural Geology with Previous HitDipNext Hit and Directional Previous HitDipNext Hit

Aqrawi, Ahmed A.*1; Boe, Trond Hellem 1
(1) Schlumberger Information Solutions, Stavanger, Norway.

We present an improved method of Previous HitdipNext Hit estimation as a seismic attribute, and visualize this in 2 components; Previous HitdipNext Hit and directional Previous HitdipNext Hit. This method proves to be very efficient in highlighting geologic structures. According to Marfurt and Chopra (1) there are several methods to estimate Previous HitdipNext Hit and they fall into three main categories; spatial and temporal derivatives, Previous HitdipNext Hit scan of most coherent Previous HitreflectorNext Hit and eigenvectors of gradient structure tensors. The method for Previous HitdipNext Hit and directional Previous HitdipNext Hit calculation looks at local weighted correlation between neighboring traces and their amplitudes, searching to maximize correlation, and therefore falls in the Martfurt et al “Previous HitdipNext Hit scan” category. Using trace to trace Previous HitdipNext Hit, it is possible to estimate either the maximal Previous HitdipNext Hit, or the Previous HitdipNext Hit in a specific direction.

Our approach, uses a gradient decent (aka hill climbing) in order to efficiently find the maximal trace to trace cross correlation. When calculating the directional Previous HitdipNext Hit, a fourth order estimate is used in both the inline and cross-line directions and a weighted sum of five estimates. When summing the five Previous HitdipNext Hit estimates in a given direction, different weightings are given to them depending on their distance from the center trace. This adds a smoothing effect and can be interpreted to less noisy results. This approach is used to calculate the Previous HitdipNext Hit in two main directions, and then this information is used to calculate the directional Previous HitdipNext Hit given an angel or the maximal Previous HitdipNext Hit, e.g. Previous HitdipNext Hit. The results prove to be very useful in detecting structural geology. Data from the Gulf of Mexico has been used to prove the methodology of the Previous HitdipNext Hit and directional Previous HitdipNext Hit calculations and shows clearly discernible salt domes, faults, and fluvial systems.

References

(1)Marfurt and Chopra (2007). Seismic attributes for prospect identification and reservoir characterization. Tulsa, OK U.S.A: Society of Exploration Geophysicists. p27-p43.

 

AAPG Search and Discovery Article #90141©2012, GEO-2012, 10th Middle East Geosciences Conference and Exhibition, 4-7 March 2012, Manama, Bahrain