Geophysikalische Untersuchung des Inntal-Untergrundes bei Thaur, östlich von Innsbruck


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Amelie.Buecker [ at ] awi.de

Abstract

A cross-section of the Inn-valley has been surveyed by refraction- and reflection-seismic and gravimetric methods. The thickness of the Inn-valley sediments is 340-390 m. At the northern edge of the valley an intermediate layer between sediments and basement has been detected, which is up to 300 m thick. This zone seems to mark the boundary of the northern calcareous alps.



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31422
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Aric, K. and Steinhauser, P. (1976): Geophysikalische Untersuchung des Inntal-Untergrundes bei Thaur, östlich von Innsbruck , Zeitschrift für Gletscherkunde und Glazialgeologie, 12 (1), pp. 37-54 .


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