1887

Abstract

The two studied, 34 and 52 km long parallel profiles are located over a gradually deepening sedimentary basin (Fig. 1). Northward these profiles terminale near the Rába Line which separates the East Alpian tectonic unit from that of the Transdanubian Central Range and the profiles are nearly perpendicular to its strike direction. Magnetotelluric profiles measured earlier over the latter tectonic unit have revealed a conductive zone within the crust.

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/content/papers/10.3997/2214-4609.201410701
1992-06-01
2020-08-07
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410701
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