Zobrazeno 1 - 10
of 20
pro vyhledávání: '"Reinhard Wolff"'
Publikováno v:
Lithosphere, Vol 2024, Iss 1 (2024)
The Eastern European Alps formed during two orogenic cycles, which took place in the Cretaceous and Cenozoic, respectively. In the Ötztal-Stubai Complex—a thrust sheet of Variscan basement and Permo-Mesozoic cover rocks—the record of the first (
Externí odkaz:
https://doaj.org/article/61cbc61443824a249ad65941fc07b037
The Austroalpine nappes in the Eastern European Alps have preserved the record of two orogenic phases in the Cretaceous and Tertiary but their cooling and exhumation history remains poorly constrained. Here we use new low-temperature thermochronologi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2e28d70034b8bca8b300a4d4b09163af
https://doi.org/10.5194/egusphere-egu23-2925
https://doi.org/10.5194/egusphere-egu23-2925
Autor:
Reinhard Wolff, Ralf Hetzel, Kyra Hölzer, István Dunkl, Qiang Xu, Aneta A. Anczkiewicz, Zhenyu Li
Publikováno v:
Journal of the Geological Society. 180
Active graben systems in south Tibet and the Himalaya are the surface expression of ongoing east–west extension, although the cause and spatiotemporal evolution of normal faulting is a still a matter of debate. We reconstructed the exhumation histo
Publikováno v:
Geomorphology. 430:108657
Publikováno v:
International Journal of Earth Sciences. 110:2955-2977
The Brenner normal fault bounds the Tauern Window to the west and accommodated a significant portion of the orogen-parallel extension in the Eastern Alps. Here, we use zircon (U–Th)/He, apatite fission track, and apatite (U–Th)/He dating, thermok
Publikováno v:
The Journal of Geology. 127:15-36
Several active graben systems in Tibet and the Himalaya are the expression of ongoing east-west extension, but the significance and history of normal faulting in this large region are still...
Autor:
Reinhard Wolff, Kyra Hölzer, Ralf Hetzel, Qiang Xu, István Dunkl, Aneta A. Anczkiewicz, Zhenyu Li
Publikováno v:
Tectonophysics. 834:229378
The northeastward motion of the Tibetan Plateau along the Altyn Tagh strike‐slip fault causes thrust faulting in three parallel mountain ranges (Qilian Shan, Daxue Shan, and Danghe Nan Shan) in the plateau interior, and leads to NNE‐directed crus
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c40aed612ccf54e8dcde4104ea73138d
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/8598
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/8598
Rapid rock exhumation in mountain belts is often associated with crustal-scale normal faulting during late-orogenic extension. The process of normal faulting advects hot footwall rocks towards the Earth's surface, which shifts isotherms upwards and i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::92518ad89d3947f1bfb1f3b951daddf3
https://doi.org/10.5194/egusphere-egu2020-2196
https://doi.org/10.5194/egusphere-egu2020-2196
Publikováno v:
Earth Surface Processes and Landforms. 43:2327-2341