Abstract

Potential-field-data imaging of complex geological features in deepwater salt-tectonic regions in the Gulf of Mexico remains an open active research field. There is still a lack of resolution in seismic imaging methods below and in the surroundings of allochthonous salt bodies. In this work, we present a novel three-dimensional potential-field-data simultaneous inversion method for imaging of salt features. This new approach incorporates a growth algorithm for source estimation, which progressively recovers geological structures by exploring a constrained parameter space; restrictions are posed from a priori geological knowledge of the study area. The algorithm is tested with synthetic data corresponding to a real complex salt-tectonic geological setting commonly found in exploration areas of deepwater Gulf of Mexico. Due to the huge amount of data involved in three-dimensional inversion of potential field data, the use of parallel computing techniques becomes mandatory. In this sense, to alleviate computational burden, an easy to implement parallelization strategy for the inversion scheme through OpenMP directives is presented. The methodology was applied to invert and integrate gravity, magnetic and full tensor gradient data of the study area.

Highlights

  • Imaging of salt-tectonic-related geological features is still a challenging research matter in geophysical exploration, in the oil exploration industry

  • The source-growth algorithm-based inversion scheme presented has shown to be an efficient method to invert the geometry of geobodies in highly complex zones such as the deepwater

  • The incorporation of Full Tensor Gradient method (FTG) data provided an excellent approximation to the geometry of salt structures and their surroundings within the study region

Read more

Summary

Introduction

Imaging of salt-tectonic-related geological features is still a challenging research matter in geophysical exploration, in the oil exploration industry. Three-dimensional seismic imaging has experienced a quite significant development in recent years [5,6,7,8,9,10], it is well known that it still tends to fail in subsalt regions due to the high-density contrasts between salt structures and their surrounding-encapsulating-rocks, yielding varying degrees of uncertainty in estimation of base and highly dipping flanks of salt bodies [11] In this context, potential field methods are often excellent supporting tools for geophysical subsalt exploration and can provide accurate estimations of depth distribution and geometry of allochthonous salt features [12,13]. Since the gradiometric tensor G is symmetric and traceless, its independent components allow determination of the locations of the mass center (Gxz , Gyz ), edges (Gyy , Gxx )

Objectives
Methods
Results
Discussion
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call