Subcrustal tectonic erosion in orogenic belts - a model for the late Cretaceous subsidence of the northern Calcareous Alps (Austria)

Autor(en)

M. Wagreich

Abstrakt

Analysis of the Upper Cretaceous to Eocene Gosau Group of the Northern Calcareous Alps (Austria) indicates rapid subsidence after a short interval of deformation, uplift, and erosion. Reconstructions of basement subsidence of >3000 m from the late Turonian (89 Ma) onward show a distinct shift of the deformation and subsidence from the northwest to the southeast together with a tilting of the Northern Calcareous Alps toward the north. Comparison with recent analogues suggest that subcrustal tectonic erosion due to the subduction of a topographic high of the South Penninic ocean may be the cause for this subsidence pattern. Tectonic erosion along ancient plate margins can be recognized by deformation and widespread erosion followed by regional subsidence not related to extension or flexural loading. -Author

Organisation(en)

Institut für Geologie

Journal

Geology

Band

21

Seiten

941-944

Anzahl der Seiten

4

ISSN

0091-7613

DOI

https://doi.org/10.1130/0091-7613(1993)021<0941:STEIOB>2.3.CO;2

Publikationsdatum

01-1993

Peer-reviewed

Ja

ÖFOS 2012

105106 Geodynamik, 105112 Historische Geologie

ASJC Scopus Sachgebiete

Geology

Link zum Portal

https://ucrisportal.univie.ac.at/de/publications/subcrustal-tectonic-erosion-in-orogenic-belts--a-model-for-the-late-cretaceous-subsidence-of-the-northern-calcareous-alps-austria(fbf78e4e-392f-4eef-9d78-b4962614936f).html