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(Article of periodic en Allemand - 1981)

Document title

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

Authors(s) and Affiliation(s)

HESSMANN W. ; SCHWANDT A. ;

Abstract

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).

Source

Article of periodic

published at : Zeitschrift für geologische Wissenschaften Berlin

Editor :

Millesime : 1981, vol. 9, no3 [pp. 283-292]

Language

Allemand

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