Abstract
Jardani et al. [2006a] (hereinafter referred to as JDR) present a self-potential survey showing circular anomalies associated with shallow sinkholes in a chalk karst. They perform various finite element modelings and data analysis, and, in particular, use a three-dimensional (3-D) version of the so-called dipole occurrence probability (DOI) tomography [Iuliano et al., 2002a].
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