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Collins, J.L., Everett, M.E. and Johnson, B. (2006) Detection of Near-Surface Horizontal Anisotropy in a Weathered Metamorphic Schist at Llano Uplift (Texas) by Transient Electromagnetic Induction. Physics of the Earth and Planetary Interiors, 158, 159-173.
http://dx.doi.org/10.1016/j.pepi.2006.05.008

has been cited by the following article:

• TITLE: Occam Inversion of Transient Electromagnetic Data in a Layered Medium with Azimuthal Anisotropy

  AUTHORS: Wangwang Wang, Changhong Lin, Handong Tan, Honglei Liu

  KEYWORDS: Azimuthal Anisotropy, Layered Medium, Occam Inversion, Horizontalelectric Dipole, Transient Electromagnetic Data

  JOURNAL NAME: International Journal of Geosciences, Vol.7 No.7, July 19, 2016

  ABSTRACT: In recent years, the anisotropic study has become a hot topic in the field of electromagnetics. Currently, inversion technologies of transient electromagnetic sounding data are mainly based on the case of an isotropic medium. However, the actual underground electrical structure tends to be complicated and anisotropic. It is often found that the isotropic inversion technologies do not lead to good results for field transient electromagnetic sounding data. We have developed an algorithm for calculating the transient electromagnetic response in a layered medium with azimuthal anisotropy. An occam inversion algorithm has also been implemented to invert the transient electromagnetic data induced by a grounded horizontal electric dipole in a layered medium with azimuthal anisotropy. Synthetic examples demonstrate the stability and validity of the inversion algorithm. Experimental results show different data for inverting have great influence on the inversion results.