Publications

Abstract not provided.

Abstract not provided.

The bulk electrical anisotropy of sedimentary formations is a macroscopic phenomenon whic h can result from the presence of sand/shale laminae and varations in grain size and pore space. Accounting for its effects on induction log response is an ongoing research problem for the w ell-logging communit y since these types of sedimentary stuctures have long been correlated with productive hydrocarbon reservoirs. Presented here is a finite difference method for sim ulatingEM induction in a fully 3D anisotropic medium. This w ork differs from previous modeling efforts in that the electrical conductivity of the formation is represented as a full 3×3 tensor whose elements can vary arbitrarily with position throughout the formation. As an example, we simulate borehole induction tool responses in a crossbedded eolian sandstone to demonstrate the challenge faced by interpreters when electrical anisotropy is neglected.