| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 9526179 | Sedimentary Geology | 2005 | 24 Pages |
Abstract
Subsidence in the study area is controlled by active strike-slip tectonics and the subsequent formation of a magmatic chamber (Predazzo/Monzoni) above the deep-reaching Truden/Stava line. The area close to this tectonic line and to the volcanic centre of Predazzo/Monzoni undergoes a higher heat flow pulse during the Late Ladinian and is possibly buried at shallower levels than the Rosengarten area. As shown by fission tracks in apatites, the heat flow pulse almost disappears laterally underlining the localised thermal influence of the Late Ladinian volcano-thermal event of Predazzo/Monzoni.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Axel Emmerich, Ulrich A. Glasmacher, Friederike Bauer, Thilo Bechstädt, Rainer Zühlke,