Abstract

The high-resolution azimuthal resistivity laterolog response in a fractured formation was numerically simulated using a three-dimensional finite element method. Simulation results show that the azimuthal resistivity is determined by fracture dipping as well as dipping direction, while the amplitude differences between deep and shallow laterolog resistivities are mainly controlled by the former. A linear relationship exists between the corrected apparent conductivities and fracture aperture. With the same fracture aperture, the deep and shallow laterolog resistivities present small values with negative separations for low-angle fractures, while azimuthal resistivities have large variations with positive separations for high-angle fractures that intersect the borehole. For dipping fractures, the variation of the azimuthal resistivity becomes larger when the fracture aperture increases. In addition, for high-angle fractures far from the borehole, a negative separation between the deep and shallow resistivities exists when fracture aperture is large as well as high resistivity contrast exists between bedrock and fracture fluid. The decreasing amplitude of dual laterolog resistivity can indicate the aperture of low-angle fractures, and the variation of the deep azimuthal resistivity can give information of the aperture of high-angle fractures and their position relative to the borehole.

Highlights

  • Fracture is the smallest and the most complex structure in the crust

  • This study aims to implement numerical simulation of the high-resolution azimuthal resistivity laterolog (HARL), in order to combine the radial detection of dual laterolog and azimuthal detection around the borehole, and corresponding logging response characteristics and identification method of fractures are investigated to aid fractured reservoir evaluation

  • Assuming that the potential distribution generated by HARL around the borehole is U, the potential gradient of bedrock can be expressed as rU, and the potential gradient in any fracture plane can be decomposed into a normal component (Ebn) and a tangential component (Ebt), which are given by

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Summary

Introduction

Fracture is the smallest and the most complex structure in the crust It can increase the pore space and permeability, and control the formation, distribution, and capacity of oil and gas in place (Jiang et al 2004; Zeng et al 2007; Zhang et al 2009; Weng et al 2011; Nie et al 2012; Kuchuk and Biryukov 2014; Reynolds et al 2014; Yao et al 2013; Zhao et al 2014). This study aims to implement numerical simulation of the high-resolution azimuthal resistivity laterolog (HARL), in order to combine the radial detection of dual laterolog and azimuthal detection around the borehole, and corresponding logging response characteristics and identification method of fractures are investigated to aid fractured reservoir evaluation

Fundamental theory
Calculation principle
Calculation condition
Relationship of HARL response and fracture dipping angle
Relationship of HARL response and fracture aperture
Azimuthal resistivity imaging of fractures
Conclusions
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