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PORTAIL D'INFORMATION GÉOGRAPHIQUE

Zur Bruchtektonik im Salinar und Deckgebirge. (La tectonique cassante dans les structures salifères et sédimentaires)

Auteurs :
HESSMANN, W.
SCHWANDT, A.

Description :
The geomechanical behaviour of certain areas of the body of salt at the caprock will be determined by the composition, the thickness and the bonding of rocks-competent or incompetent areas of the rocks. In general, the structural deformation of salt rock by solide state flowing is contrasted by a deformation of the regional overburden resulting from fracturing tectonics. As model conceptions prove, both the alpine structure of salt body and the germanotype mosaic of fault blocks of the overburden are results of the still lasting evolutionary process as to tectonics ans structure which started at the sedimentation in the Permian-Mesozoic age and is characterized by changing activities and intensities. (d'après HL).


Type de document :
Article de périodique

Source :
Zeitschrift für geologische Wissenschaften Berlin, 1981, vol. 9, n°. 3, p. 283-292

Date :
1981

Langue :
Allemand
Droits :
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