Tab. 2: Gravity measurements of the Inntal underground at Thaur
| Cobertura |
MEDIAN LATITUDE: 11.468768 * MEDIAN LONGITUDE: 47.281384 * SOUTH-BOUND LATITUDE: 11.452600 * WEST-BOUND LONGITUDE: 47.237600 * NORTH-BOUND LATITUDE: 11.474200 * EAST-BOUND LONGITUDE: 47.308300 * MINIMUM ELEVATION: 562.90 m a.s.l. * MAXIMUM ELEVATION: 972.70 m a.s.l. |
|---|---|
| Data(s) |
14/12/1976
|
| Resumo |
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. |
| Formato |
text/tab-separated-values, 114 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.804212 doi:10.1594/PANGAEA.804212 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Fonte |
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, hdl:10013/epic.40216.d001 |
| Palavras-Chave | #Bouguer anomaly; delta; ELEVATION; Free-air gravity anomaly; Gravity; LATITUDE; LONGITUDE; Number; Thaur; Thaur, Innsbruck Land, Tyrol, Austria |
| Tipo |
Dataset |
