Tab. 2: Gravity measurements of the Inntal underground at Thaur

Dataset

DOI PID

A cross-section of the Inn-valley has been surveyed by refraction- and refiection-seismic and gravimetrie methods. The thickness of the Inn-va.!ley 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 ITl thick. This zone seems to mark the boundary of the northern calcareous alps.

Supplement to: Aric, Kay; Steinhauser, Peter (1976): Geophysikalische Untersuchung des Inntal-Untergrundes bei Thaur, östlich von Innsbruck. Zeitschrift für Gletscherkunde und Glazialgeologie, 12(1), 37-54

Identifier
DOI	https://doi.org/10.1594/PANGAEA.804212
PID	https://hdl.handle.net/10013/epic.40216.d001
Metadata Access	https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.804212

Provenance
Creator	Aric, Kay; Steinhauser, Peter
Publisher	PANGAEA
Publication Year	1976
Rights	Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess	true

Representation
Resource Type	Supplementary Dataset; Dataset
Format	text/tab-separated-values
Size	114 data points
Discipline	Earth System Research
Spatial Coverage	(47.238W, 11.453S, 47.308E, 11.474N); Thaur, Innsbruck Land, Tyrol, Austria