Relative space-time scaling of electromagnetic soundings arrays

Abstract

There are many methods for the study of near-surface applied geophysics. This study will not only help understand how the main geoelectrical methods works (DC and MT) but also improve the technique used for analysis, combining the best of both methods and takes advantage of the best each. I test an empirical relation between the DC and MT data on synthetic models and I applied it on real data. A discussion of the limits and utility of this relationship is also presented.