Zobrazeno 1 - 10
of 34
pro vyhledávání: '"Jan Pleuger"'
Publikováno v:
Swiss Journal of Geosciences, Vol 115, Iss 1, Pp 1-40 (2022)
Abstract Continent-derived tectonic units in the Tauern Window of the Alps exhibit stratigraphic and structural traces of extension of continental margins eventually leading to the opening of the Alpine Tethys. In this study, we reassess lithostratig
Externí odkaz:
https://doaj.org/article/e9eab48463d04155bb354c7314ad4627
Autor:
Olga Brunsmann, Marisa Germer, Alexandra Pohl, Victoria Kohn, Vincent Könemann, Xin Zhong, Jan Pleuger, Timm John
The Adula nappe in the Swiss-Italian Central Alps is a continental basement nappe from the former European margin that was subducted to depths indicating (ultra)-high-pressure conditions. Many studies were performed to understand the pressure-tempera
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dbdf23967f564dc5e6de4ea3e4bbfcd4
https://doi.org/10.5194/egusphere-alpshop2022-33
https://doi.org/10.5194/egusphere-alpshop2022-33
The Koralpe-Saualpe-Pohorje Complex in the Eastern Alps represents a lithologically heterogenous (U)HP nappe with eclogite lenses embedded in gneissic and metasedimentary rocks. The aim of this project is to determine whether or not tectonic pressure
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b684a65b52e496d318c6ab319ae7933e
https://doi.org/10.5194/egusphere-alpshop2022-42
https://doi.org/10.5194/egusphere-alpshop2022-42
Publikováno v:
Earth and Planetary Science Letters
The tectonic structure of the Eastern Alps is heavily debated with successive geophysical studies that are unable to resolve areas of ambiguity (e.g., the presence of a switch in subduction polarity and differing crustal models). In order to better u
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::96c950187baf15053c7f5baf167595c9
https://doi.org/10.1016/j.epsl.2023.118096
https://doi.org/10.1016/j.epsl.2023.118096
Publikováno v:
Journal of Metamorphic Geology. 39:247-269
We investigate the evolution of the three‐dimensional thermal structure of a palaeo‐subduction channel exposed in the Penninic units of the central Tauern Window (Eastern Alps). Structural and petrological observations reveal a sheath fold with a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3428bab9a26798adddef5be1153fa789
https://doi.org/10.1111/jmg.12572
https://doi.org/10.1111/jmg.12572
Autor:
Xin Zhong, Marisa Germer, Alexandra Pohl, Vincent Könemann, Olga Brunsmann, Philip Groß, Jan Pleuger, Timm John
The Adula nappe is located at the eastern flank of the Lepontine dome in the Swiss Alps. It consists mainly of orthogneiss and paragneiss with intercalated lenses of eclogite, amphibolite and metasediments. Previous petrological studies on the peak p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ce0bbdea3f13d6dfb41d68541a385a00
https://doi.org/10.5194/egusphere-egu22-8422
https://doi.org/10.5194/egusphere-egu22-8422
The junction between the Dinarides and the Hellenides coincides with an orogenic bend characterized by a complex system of faults, domes and sedimentary basins. The major structure at this junction is the Shkoder-Peja Normal Fault (SPNF) system, whic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d6d34a139f01ae5824fd949cc7ffddde
https://doi.org/10.5194/egusphere-egu21-14816
https://doi.org/10.5194/egusphere-egu21-14816
The dense SWATH-D seismic network in the Central-Eastern Alps gives an unprecedented window into the collision of the Adriatic and European plates. Previous studies have suggested a Moho gap overlying a subduction polarity switch. This switch, from E
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::34e0c77291f765f5998eb82b9d2ed989
https://doi.org/10.5194/egusphere-egu21-11044
https://doi.org/10.5194/egusphere-egu21-11044
Knowledge on the thermal state of orogens and subduction zones is crucial in trying to understand the processes that take place in these zones, since temperature controls, e.g., rock strength, metamorphic reactions and fluid flow. These are all criti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::43e47b22afd067c232626947004b2e3b
https://doi.org/10.5194/egusphere-egu2020-8054
https://doi.org/10.5194/egusphere-egu2020-8054
In the Eastern Alps, teleseismic tomography suggests that there is a switch from European subduction in the west to Adriatic subduction in the east. The dense SWATH-D seismic network is located in the central-eastern Alps between around 10°E and 14.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c62267f2d7278581774b80bcd96812c6
https://doi.org/10.5194/egusphere-egu2020-13785
https://doi.org/10.5194/egusphere-egu2020-13785