Zobrazeno 1 - 10
of 29
pro vyhledávání: '"Christoph Iglseder"'
Publikováno v:
Swiss Journal of Geosciences, Vol 117, Iss 1, Pp 1-25 (2024)
Abstract The Troiseck-Floning and Rosskogel nappes are part of the Austroalpine Unit in the eastern part of the Eastern Alps. The nappes are in tectonic contact and comprise Permian to Mesozoic lower greenschist facies metamorphic metasediments, but
Externí odkaz:
https://doaj.org/article/f5541a339eac4ce98867168f10e7cdb5
The affiliation of the Ennstal Phyllite Zone (EPZ) to either the micaschist units of the Koralpe-Wölz nappe system (KW-NS) to its south or to nappes of the “Greywacke Zone” to its north and east is still debated. Due to similarities with phyllit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f1c32d762da2c083858e09694fe5989e
https://doi.org/10.5194/egusphere-egu23-8495
https://doi.org/10.5194/egusphere-egu23-8495
The Ötztal-Nappe in the central Eastern Alps represents a classical area of polyphase deformation and metamorphism. The pre-Mesozoic basement (Ötztal-Stubai Complex; OSC) comprises metasediments (paragneiss and mica schist), metaigneous rocks and m
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fb5d09d33b13510b1915118fe0ba0944
https://doi.org/10.5194/egusphere-alpshop2022-52
https://doi.org/10.5194/egusphere-alpshop2022-52
This contribution reports LA-ICP-MS zircon ages and Rb-Sr biotite ages from the Troiseck-Floning Nappe, forming the northeasternmost extension of the Silvretta-Seckau Nappe System in the Eastern Alps. The Troiseck-Floning Nappe comprises a basement f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b9fc1bb3230543a68b57db5576683391
https://doi.org/10.5194/egusphere-alpshop2022-12
https://doi.org/10.5194/egusphere-alpshop2022-12
Autor:
Marianne Sophie Hollinetz, Ralf Schuster, Manuel Werdenich, Benjamin Huet, Gerd Rantitsch, Christoph Iglseder
Publikováno v:
International Journal of Earth Sciences. 109:2235-2253
At the northwestern margin of the Gurktal Alps (Eastern Alps), Eoalpine (Cretaceous) thrusting of carbonaceous material (CM) bearing metasediments formed a very low- to low-grade metamorphic nappe stack above higher-grade metamorphic basement nappes.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::76da166a6feaee9725b02bb8fac2e2cb
https://doi.org/10.1007/s00531-020-01897-7
https://doi.org/10.1007/s00531-020-01897-7
Publikováno v:
Austrian Journal of Earth Sciences. 113:139-153
This work describes the Freyenstein Fault System, which extends over 45 km in the southeastern part of the Bohemian Massif (Lower Austria). It represents a ductile shear zone overprinted by a brittle fault located at the eastern edge of the South Boh
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a0615e554565a0cc2dc6095347427732
https://doi.org/10.17738/ajes.2020.0009
https://doi.org/10.17738/ajes.2020.0009
Based on new structural field data and Raman micro-spectroscopy on carbonaceous material a major detachment juxtaposing Drauzug-Gurktal Nappe System (DGN) against the transgressive Permo-Mesozoic cover sequence of the Ötztal-Bundschuh Nappe System (
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::826894f74bdb8cbdbe56815e298aaaf6
https://doi.org/10.5194/egusphere-egu2020-19144
https://doi.org/10.5194/egusphere-egu2020-19144
Publikováno v:
Journal of Petrology. 59:1359-1382
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8bb41a2d8713c26f439a2da4e363a7e2
https://doi.org/10.1093/petrology/egy063
https://doi.org/10.1093/petrology/egy063
Publikováno v:
Lithosphere. 4:23-39
Current models for Miocene backarc extension of the Aegean region generally suggest that stretching was accommodated mainly by NE-dipping low-angle normal faults with N to NE sense of shear. A crustal-scale low-angle normal fault system trending over
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a2b0e503632a9f715b426d6b4a3ddee6
https://doi.org/10.1130/l164.1
https://doi.org/10.1130/l164.1
Autor:
Bernhard Grasemann, David A. Schneider, Konstantin Petrakakis, Urs Klötzli, Christoph Iglseder, András Zámolyi, C. Miller, C. Rambousek, Martin Thöni
Publikováno v:
Tectonophysics. 473:69-83
Tertiary I- and S-type plutonism is widespread in the Aegean region and frequently associated with extensional tectonic structures. This investigation presents the first evidence of protracted magmatism on the island of Serifos in the western Cyclade
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d240aa57c8330542120952becf332fb9
https://doi.org/10.1016/j.tecto.2008.09.021
https://doi.org/10.1016/j.tecto.2008.09.021