Top Qs
Timeline
Chat
Perspective
Giessen nappe
From Wikipedia, the free encyclopedia
Remove ads
The Giessen nappe (German: Gießener Decke) is a tectonic nappe in the southeastern part of the Rhenish Massif in western Germany. The nappe is an "alien" (allochthonous) unit in the Rhenohercynian zone of the Hercynian orogeny, it was thrust over the usual slightly metamorphosed Devonian and Carboniferous sedimentary rocks in this zone.[1]

The Giessen nappe is often correlated with the Harz nappe in the Harz[2] and similar units in the Bohemian Massif in the Czech Republic.[3] These units form the rare erosional leftovers of small microcontinents that were during the Hercynian orogeny squeezed between the paleocontinents Gondwana to the south and Laurussia to the north.
Remove ads
Outcrop area
Giessen nappe outcrops cover about 300 km2 from the western edge of the Vogelsberg over Braunfels, Wetzlar and Gießen, almost to Marburg. The river Lahn flows along the northern part of the nappe until it crosses the nappe between Gießen and Wetzlar to continue flowing westwards to the Rhine.
Lithology and stratigraphy
Wikiwand - on
Seamless Wikipedia browsing. On steroids.
Remove ads