It has been studied whether the deep fractures detected by magnetotelluric soundings along the longitudinal strike slips in the NE-SW direction can be followed on the surface (in the tectonic maps), further on are they continuously open (loosed) in their total length or not. In this latter case they consist of a series of conducting dikes arranged along the main tectonic directions. In the generation of these dikes the crossing of the longitudinal and transversal fractures can play the decisive role. The telluric map(s) and the magnetotelluric and magnetovariation profile seem to confirm the latter statement.
|Number of pages||10|
|Publication status||Published - Jan 1 2003|
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