Shelfkruste und Drift. Konsequente Fortsetzung der von Bubnoffschen Aussagen. (Croûte continentale et dérive. Approfondissement des travaux de von Bubnoff)

Auteur :
BRAUSE, H.

Description :
According to v. Bubnoff, the varied substructure is the cause for the different mobility behaviour. The types of crustal structure correspond to original arrangements of formation of the earth's crust. As an original arrangement, in addition to shields, the type of the shelf crust exists, as illustrated by Central and Western Europe. The geosynclinal, tectogenetic and magmatic development conditioned by the drift in this shelf crust region is described in outline. The geotectonic events are considered to be part of global processes. The drift stop at the end of the Palaeozoid epoch led to revolutionary changes in the system of global rotation, the major break in the evolution of life at the Permian-Triassic boundary being one of its sequels.


Type de document :
Article de périodique

Source :
Zeitschrift für geologische Wissenschaften Berlin, 1979, vol. 7, n°. 2, p. 183-191

Date :
1979