English
 
Privacy Policy Disclaimer
  Advanced SearchBrowse

Item

ITEM ACTIONSEXPORT
Add to Basket
  Local TagsRelease HistoryDetailsSummary

Released
Journal Article

A high-velocity layer in the lower crust of the North German Basin

Authors

Rabbel,  W.
External Organizations;

Förste,  K.
External Organizations;

/persons/resource/robert

Schulze,  Albrecht
Deutsches GeoForschungsZentrum;

Bittner,  R.
External Organizations;

Röhl,  J.
External Organizations;

Reichert,  J. C.
External Organizations;

, 

External Ressource
No external resources are shared
Fulltext (public)
There are no public fulltexts stored in GFZpublic
Supplementary Material (public)
There is no public supplementary material available
Citation

Rabbel, W., Förste, K., Schulze, A., Bittner, R., Röhl, J., Reichert, J. C. (1995): A high-velocity layer in the lower crust of the North German Basin. - Terra Nova, 7, 3, 327-337.
https://doi.org/10.1111/j.1365-3121.1995.tb00802.x


https://gfzpublic.gfz-potsdam.de/pubman/item/item_237230
Abstract
A network of deep seismic refraction profiles in Northern Germany consisting of parts of the European Geotraverse (EGT) and additional new lines is interpreted. The most striking result is the proof of an approximately 10 km thick high-velocity layer in the lower crust. Its P-wave velocity of 6.9-7.5 km s(hoch)-1 is typical for shield crusts of lower crust in extensional environments intruded by mafic magma. The layer is observed in an area of roughly 150 x 180 km north of the Elbe river and seems to continue north-east, at least up to the Caledonian deformation front at the southern edge of the Ringkøbing-Fyn High. It correlates spatially with an area of high positive gravity anomalies. Here, a Moho topography of several kilometers, which had already been postulated on the basis of gravity inversions and sporadic near-vertical P(tief)M P reflections, could be confirmed by the interpretation of seismic wide-angle records. The termination of the high-velocity lower crust at the Lower Elbe Lineament, which strikes parallel to the Teisseyre-Tornquist Zone, contributes to its definition as a major lineament in the context of central European tectonics.