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

Aric, Kay and Steinhauser, Peter ;

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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.

Item Type

Article

Authors

Aric, Kay and Steinhauser, Peter ;

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Non-AWI items

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Basic Research > Helmholtz Independent Research

Publication Status

Published

Eprint ID

31422

Cite as

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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Cite this document as:

hdl:10013/epic.40216.d001

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