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One of the Penninic Nappes is the Kőszeg-Rechnitz (K-R) tectonic window at the Eastern end of the Eastern Alps. It has a complicated metamorphic history from the Jurassic time. The organic material of the Penninic Ocean was transformed to electrically conductive meta-anthracite. Its amount in the chalcophyllite is estimated by geochemists to 0.2 per cent. \udTaking this conducting structure as a test area pilot deep magnetotelluric (MT) soundings have been carried out and we determined\ud-	the structure of the conductivity anomaly due to 0.2 per cent meta anthracite in the K-R window and its surroundings\ud-	the different kinds of MT distortions as lateral (side) effect of the conductor appearing in the crust and mantle\ud-	the most probable depth of the conductive asthenosphere at the border of the Pannonian Basin (having extreme shallow asthenosphere). The obtained ~140 km depth is in correlation with value of the asthenospheric map based mainly on seismic data.\u

Indication of meta-anthracite by magnetotellurics in the Kőszeg-Rechnitz Penninic window: a test area