Subhercyn

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Under Subherzyn is - especially in the geology of northern - Harzvorland understood. Geologically it is viewed as a subhercyne depression and is a subsidence structure in the western part of the Saxon-Thuringian plaice, which is limited by structural zones and faults . It forms a floe mosaic , the partial floes of which were adjusted against each other during the Cimmerian and Alpid mountain formation , and is spread to the north and northeast through the Flechtingen-Roßlauer floe , to the east through the Wittenberger floe, to the south-east through the Halle-Hettstedter mountain bridge and to the south through the Resin clod limited.

literature

• Gerhard Patzelt: Northern Harz foreland . (= Collection of Geological Guides, Volume 96) Brothers Borntraeger, 2003

Individual evidence

1. ↑ G. Ehmke, G. Katzung: The pretertiary in East Germany. Sven von Loga, Cologne 1993, 139 pp.
2. ^ F. Kockel (ed.): Geotectonic Atlas of NW Germany. BGR Hanover 1996
3. ↑ F. Eberhardt: Geological structure and natural gas flow of the subhercyneal basin. Dissertation, Bergakademie Freiberg 1969, 161 pp.
4. ↑ Peter Balaske: The marine influenced sands in the Tertiary of Nachterstedt-Schadeleben in the eastern subhercyneal depression - sedimentology, facies and stratigraphic evaluation . Dissertation, Martin Luther University Halle-Wittenberg, 1998.