Titlebook: Strain Facies; Edward Hansen Book 1971 Springer-Verlag Berlin Heidelberg 1971 Falte.Strain.Tektonische Fazies.Trollheimen /Geologie.enviro

盘旋

Geometric Types of Flow,n chains result from the transport and flow of large volumes of rock. Mesoscopic structures displaying the same style, symmetry, and orientation of principal fabric axes as the macroscopic structures in which they are found indicate that the large-scale flow was penetrative to the mesoscopic scale.

Cirrhosis

,Trollheimen’s Rock Units,was named the Trollhetta granite by . (1938, p. 50) for its occurrence in Trollhetta, a peak located less than a kilometer north of the area mapped. The quartzite sequence is called the Gjevilvatn group because of its good exposure in the southwestern part of the area along Gjevilvatnet and upon the

Sigmoidoscopy

The Sahlfold Facies, consisting primarily of flagstone, is drawn in black. The sections show the general forms and relative locations of the major structural complexes in southeastern Trollheimen: Svarthammer anticline, the eastern homocline, and Riar basin. Structures in the rocks east of Svarthammer anticline are dis

Recess

The Discfold Facies,g. 66), but its complexity varies drastically and discontinuously across strike. To the west it is relatively simple. As one walks from the crest of Svarthammer anticline on Falkfangerhø eastward to Tyrikvamfjellet and Høghø, one passes steadily upward in the rock column from flagstone of the Indre

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