Abstract

The identification of small scale faults (SSFs) and fractures provides an improved understanding of geologic structural features and can be exploited for future drilling prospects. Conventional SSF and fracture characterization are challenging and time-consuming. Thus, the current study was conducted with the following aims: (a) to provide an effective way of utilizing the seismic data in the absence of image logs and cores for characterizing SSFs and fractures; (b) to present an unconventional way of data conditioning using geostatistical and structural filtering; (c) to provide an advanced workflow through multi-attributes, neural networks, and ant-colony optimization (ACO) for the recognition of fracture networks; and (d) to identify the fault and fracture orientation parameters within the study area. Initially, a steering cube was generated, and a dip-steered median filter (DSMF), a dip-steered diffusion filter (DSDF), and a fault enhancement filter (FEF) were applied to sharpen the discontinuities. Multiple structural attributes were applied and shortlisted, including dip and curvature attributes, filtered and unfiltered similarity attributes, thinned fault likelihood (TFL), fracture density, and fracture proximity. These shortlisted attributes were computed through unsupervised vector quantization (UVQ) neural networks. The results of the UVQ revealed the orientations, locations, and extensions of fractures in the study area. The ACO proved helpful in identifying the fracture parameters such as fracture length, dip angle, azimuth, and surface area. The adopted workflow also revealed a small scale fault which had an NNW–SSE orientation with minor heave and throw. The implemented workflow of structural interpretation is helpful for the field development of the study area and can be applied worldwide in carbonate, sand, coal, and shale gas fields.

Highlights

  • Small scale faults (SSFs) are responsible for a minor portion of all seismic activity in an active region and have an offset of about 25–50 m [1] that can extend to about 2–4 km with small throws ofAppl

  • The methods applied in the study for the delineation of the small scale faults and fractures incorporated the combined use of data conditioning, multi-attribute analysis, artificial neural networks (ANNs), and the ant-colony optimization (ACO) approach

  • The results provided a comparison of the original seismic (Figure 3a), dip-steered median filter (Figure 3b), dip-steered diffusion filter (Figure 3c), and the fault enhancement filter (Figure 3d) at inline 665

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Summary

Introduction

Small scale faults (SSFs) are responsible for a minor portion of all seismic activity in an active region and have an offset of about 25–50 m [1] that can extend to about 2–4 km with small throws of. Afterwards, artificial neural networks (ANNs) were applied to these attributes to characterize the fracture network These seismic attributes provided the basis for detecting small scale reflection continuities in the seismic data, which is difficult to do when using conventional interpretation techniques. The current study aimed to identify the small scale fault and network of fractures in reservoir sands using 3D seismic data within the Sawan gas field of the Lower Indus Basin, which has been previously overlooked. The methods applied in the study for the delineation of the small scale faults and fractures incorporated the combined use of data conditioning, multi-attribute analysis (using dip, curvature, variance, similarity, thinned-fault likelihood, fracture density, and fracture proximity), ANNs, and the ACO approach. The applied ant-colony optimization algorithm was followed by the automatic fault extraction technology to reveal the dip azimuth, dip angle, fracture length, and surface area of the fractures

Geological Settings
Methodology
Artificial
Ant-Colony Optimization
Fault and Fracture Extraction
Seismic Conditioning
Seismic
Shortlisting
Curvature
Similarity
It generates seismic volumes with as aapower it has a range between
The inserted on the resultant
Thinned-fault
Fracture
Fracture Proximity
Fracture Density
Neural
Attribute Conditioning
Structural Smoothing
Variance
Ant-Tracking Result
Automatic Fault and Fracture Extraction Using ACO
Conclusions
Full Text
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