Zobrazeno 1 - 10
of 22
pro vyhledávání: '"Aneta A. Anczkiewicz"'
Autor:
Tomasz Powolny, Magdalena Dumańska-Słowik, Aneta A. Anczkiewicz, Magdalena Sikorska-Jaworowska
Publikováno v:
Scientific Reports, Vol 12, Iss 1, Pp 1-26 (2022)
Abstract The formation of spilitic assemblages (i.e. chlorite and albite) has been ubiquitously involved during the evolution of continental early-Permian volcanics from the Intra-Sudetic Basin (ISB). Based on the investigation of laccolith-type and
Externí odkaz:
https://doaj.org/article/523fd60b21334ccba4bfa9b545ac320c
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5b37dfb08761df774f095932f8480a1a
https://doi.org/10.1144/jgs2022-090
https://doi.org/10.1144/jgs2022-090
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::92810726a5fa1ae5581f3e5b3991df4a
https://doi.org/10.1007/s00531-021-02094-w
https://doi.org/10.1007/s00531-021-02094-w
Publikováno v:
Solid Earth, Vol 12, Pp 1899-1930 (2021)
The Phanerozoic tectonothermal evolution of the SW slope of the East European Platform (EEP) in Poland is reconstructed by means of thermal maturity, low-temperature thermochronometry, and thermal modelling. We provide a set of new thermochronometric
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::80d0d131f5716fc04b9a867f1799818d
https://se.copernicus.org/articles/12/1899/2021/
https://se.copernicus.org/articles/12/1899/2021/
Publikováno v:
International Journal of Earth Sciences. 108:2561-2576
The Intra-Sudetic Basin, a ~ 12 km deep Variscan intramontane basin, has the best preserved post-orogenic sedimentary record available at the NE margin of the Bohemian Massif. Apatite fission track (AFT) analyses have been performed on 16 sedimentary
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::52af1bc46a84c2f5d7e9b3d31222bacb
https://doi.org/10.1007/s00531-019-01777-9
https://doi.org/10.1007/s00531-019-01777-9
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...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0d0207b6718d6ea03711bcbef9017a4b
https://doi.org/10.1086/700406
https://doi.org/10.1086/700406
Autor:
Reinhard Wolff, Kyra Hölzer, Ralf Hetzel, Qiang Xu, István Dunkl, Aneta A. Anczkiewicz, Zhenyu Li
Publikováno v:
Tectonophysics. 834:229378
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3ec9eb0f8f792eb69de263499a9ac3ba
https://doi.org/10.1016/j.tecto.2022.229378
https://doi.org/10.1016/j.tecto.2022.229378
The Phanerozoic tectono-thermal evolution of the SW slope of the East European Platform (EEP) in Poland is reconstructed by means of thermal maturity, low temperature thermochronometry and thermal modelling. We provide a set of new thermochronometric
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c5cbda98f72550b4c75156403706a12b
https://doi.org/10.5194/se-2021-8
https://doi.org/10.5194/se-2021-8
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
Autor:
Jan Środoń, Hilmar von Eynatten, Aneta A. Anczkiewicz, Michał Banaś, Bruno Tomljenović, Igor Vlahović, István Dunkl, Tadeusz Kawiak, Ivo Velić
Publikováno v:
Tectonophysics. 744:155-176
This study was undertaken to obtain the first thermochronological and clay mineralogy data to unravel the thermal history (maximum temperatures, timing, origin of the temperature increase, rate of exhumation) of the central part of the Karst Dinaride
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9e8962615f4857f60c1e544e848f0920
https://doi.org/10.1016/j.tecto.2018.06.016
https://doi.org/10.1016/j.tecto.2018.06.016