Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
9527085 | Tectonophysics | 2005 | 14 Pages |
Abstract
The data indeed point toward a control of post-Permian evolution by gradual withdrawal of salt triggered by the initial exhaustion along the Triassic subsidence centre. In this sense, the Glueckstadt Graben was formed at least partially as “basin scale rim syncline” during post-Permian times. The present day Hamburger, East and Westholstein Troughs are the actual final state of this long-term process which still may continue and may play a role in terms of young processes and, e.g., for coastal protection.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Yuriy Maystrenko, Ulf Bayer, Magdalena Scheck-Wenderoth,