Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Sandra Braumann"'
Autor:
Stephanie Neuhuber, Zsófia Ruszkiczay-Rüdiger, Régis Braucher, Bernhard Salcher, Esther Hintersberger, Wolfgang Thöny, Philipp Strauss, Sabine Grupe, Thomas Payer, Sandra Braumann, Christopher Lüthgens, Markus Fiebig
Quaternary landscape evolution in the Vienna Basin and the adjacent area west of its subsiding area is controlled by sediment redeposition, aggradation and erosion of the Danube, local normal faulting, and overall regional uplift. Glacial - interglac
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5ed893ae14a384d87ccf07391e1df6bb
https://doi.org/10.5194/egusphere-egu23-11536
https://doi.org/10.5194/egusphere-egu23-11536
Autor:
Joerg M. Schaefer, Stephanie Neuhuber, Sandra Braumann, Markus Fiebig, Christopher Lüthgens, Alan J. Hidy
Publikováno v:
Climate of the Past, Vol 17, Pp 2451-2479 (2021)
Glaciers preserve climate variations in their geological and geomorphological records, which makes them prime candidates for climate reconstructions. Investigating the glacier–climate system over the past millennia is particularly relevant first be
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7aec1ac7672d6aeef971043827d381d6
https://cp.copernicus.org/preprints/cp-2021-54/
https://cp.copernicus.org/preprints/cp-2021-54/
Autor:
Mads Faurschou Knudsen, Zsófia Ruszkizcay-Rüdiger, Philipp Häuselmann, Sandra Braumann, Markus Feibig, Jesper Nørgaard, John D. Jansen, Stephanie Neuhuber
For sediment-burial dating with a cosmogenic nuclide pair, the isochron burial method performs well provided that the sediment source has undergone (1) steady erosion and (2) continuous exposure to cosmic rays. These conditions exert important limita
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1d7f8048364e7958ef672284bee4893d
https://doi.org/10.5194/egusphere-egu21-14848
https://doi.org/10.5194/egusphere-egu21-14848
Mountain glaciers and their preserved moraine records provide important insights into periods when climate conditions favored glacier advance or stabilization. Comprehensive mapping of moraines in glacier forefields elucidates the spatial distributio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8fb461b72ee31c2488c9ba81e58950f3
https://doi.org/10.5194/egusphere-egu21-11494
https://doi.org/10.5194/egusphere-egu21-11494
Autor:
Markus Fiebig, Klaus Voit, Christopher Lüthgens, Sandra Braumann, Stephanie Neuhuber, Lukas Plan, Johannes Lachner, Fabian Bodenlenz, Esther Hintersberger, Suzanne Gier, Denis Scholz
The abstract is available here: https://uscholar.univie.ac.at/o:1227620
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::80e290cc6a3e93bff34ab2525869d4f8
https://phaidra.univie.ac.at/o:1227620
https://phaidra.univie.ac.at/o:1227620
Autor:
Denis Scholz, Johannes Lachner, Christopher Lüthgens, Lukas Plan, Sandra Braumann, Esther Hintersberger, Stephanie Neuhuber, Susanne Gier, Markus Fiebig
The Hainburg Hills form an elevated range at the south of the Male Karpaty mountains and separate the Vienna Basin from the Danube Basin. They consist of Variscian magmatic and metamorphic rocks covered with anchimetamorphic Mesozoic carbonates. The
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1861732bac7da0167bbe591f5ef2262b
https://doi.org/10.5194/egusphere-egu2020-7098
https://doi.org/10.5194/egusphere-egu2020-7098
Autor:
Stephanie Neuhuber, Zsófia Ruszkiczay-Rüdiger, Christopher Lüthgens, Philip Martin, Bernhard Salcher, Esther Hintersberger, Régis Braucher, Johannes Lachner, Sandra Braumann, Markus Fiebig
Fluvial terraces within the extensional structure of the Vienna Basin have been dissected by faults related to the sinistral movement of the Vienna Basin Transform Fault System (VBTF, Decker et al., 2005). Each fault block within the basin displays a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::30edd2eb85aeedc7182043045467b2c8
https://doi.org/10.5194/egusphere-egu2020-11034
https://doi.org/10.5194/egusphere-egu2020-11034
Autor:
Christopher Lüthgens, Jürgen M. Reitner, Stephanie Neuhuber, Sandra Braumann, Markus Fiebig, Joerg M. Schaefer
Publikováno v:
Quaternary Science Reviews. 245:106493
Mountain glaciers are important water resources in Alpine regions and are sensitive to climate change. Reconstructing glacier oscillations improves our understanding of the amplitude and the frequency of climate variability and resolves time periods