--> Perdido Reimaging: Overview of Model Building and Imaging Challenges and Solutions
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AAPG ACE 2018

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Perdido Reimaging: Overview of Model Building and Previous HitImagingNext Hit Previous HitChallengesNext Hit and Previous HitSolutionsNext Hit

Abstract

Summary

We present an overview of Previous HitchallengesNext Hit and Previous HitsolutionsNext Hit for Perdido reimaging, a depth-Previous HitimagingNext Hit project located over the southern Perdido Fold Belt, Salina del Bravo province, subsalt belt and adjacent inboard and outboard areas, in the western Gulf of Mexico. Geology within this 40,000 sq. km area comprises not only complex allochthonous salt and subsalt structures but also pervasive, complex shale, both in a setting that has undergone multiple compressional regimes. Given these geological Previous HitchallengesNext Hit for Previous HitimagingNext Hit, a multidiscipline approach is proposed to provide Previous HitsolutionsNext Hit for earth model building to improve image quality for regional subsurface mapping as well as for Previous HithydrocarbonNext Hit exploration. Key geophysical techniques include broadband deghosting, utilization of gravity measurements and modeling for salt interpretation, integrating borehole information, multi-azimuth tomography, as well as both refraction and reflection full-waveform inversion.

Applications

The same geological aspects that make Previous HithydrocarbonNext Hit exploration in this region conceivable also pose significant Previous HitchallengesNext Hit for velocity modeling and Previous HitimagingTop. Our workflow leverages both well-established methods and more recent technologies. Early and consisent usage of stratigraphic mapping and petro-physical analysis is key to guiding and validating model updates in complex compressional zones that exhibit large spatial and depth variability in velocity. In combination, tomography and full-waveform inversion can provide robust bulk model updates over a regional setting, shallow to deep, even starting from a simple 1D function. Gravity information proved not only useful for assessing interpretation error in the massive, amalgamated canopies of the Salina del Bravo, but also for discerning other potential errors in the larger earth model, such as the thick shale, elevated Mesozoic strata, and autochthonous salt presence.

Conclusions

We employed a multi-measurement workflow for this region through which allowed us to resolve a more accurate earth model. The workflow includes a multifaceted approach to the velocity update for shale, salt & subsalt. We demonstrate that with this strategy, significant image uplift can be achieved through Kirchhoff depth and reverse time migrations over legacy volumes.