Zobrazeno 1 - 10
of 47
pro vyhledávání: '"Diethard Sanders"'
Publikováno v:
Austrian Journal of Earth Sciences. 115:74-99
The Gosau Group (Turonian to Ypresian) of the Eastern Alps is a synorogenic wedge-top succession that accumulated in active depocenters in an oblique-convergent plate tectonic setting. Due to high morphological differentiation of depocenters by tecto
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a760f74d908403f3a785d238bb1adc3f
https://doi.org/10.17738/ajes.2022.0004
https://doi.org/10.17738/ajes.2022.0004
Publikováno v:
Austrian Journal of Earth Sciences. 115:167-190
Deformation affecting the Upper Triassic Dachstein Limestone has been analyzed in the Dachstein thrust sheet, the uppermost thrust unit of the central Northern Calcareous Alps (Eastern Alps). Different scales of deformation are discussed, from kilome
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::36e12e8fc93fbdad81d75acad728aaa4
https://doi.org/10.17738/ajes.2022.0008
https://doi.org/10.17738/ajes.2022.0008
Publikováno v:
Nova Hedwigia
It is often difficult to decide which cyanobacteria found in endolithic habitats of calcite spring-tufa deposits are present as ephemeral components of the biota or are persistent, structural elements. To answer this question, we repeatedly studied t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ed048894f96f41a12a21cf7453127218
https://doi.org/10.1127/nova_hedwigia/2021/0615
https://doi.org/10.1127/nova_hedwigia/2021/0615
Publikováno v:
Geomorphology. 413:108350
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d9df48769d41d03f334f26325028f043
https://doi.org/10.1016/j.geomorph.2022.108350
https://doi.org/10.1016/j.geomorph.2022.108350
Publikováno v:
Austrian Journal of Earth Sciences. 111:180-203
In intramontane landscapes shaped by glacial-interglacial cycles, the most rapid changes during the proglacial/paraglacial phases may be amplified by catastrophic mass-wasting. Herein, we describe the Last Glacial Maximum (LGM) to Holocene developmen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3913a740e91168ed0090b5d1e256a4ea
https://doi.org/10.17738/ajes.2018.0012
https://doi.org/10.17738/ajes.2018.0012
The Tsergo Ri rockslide represents one of the world's biggest rockslides in crystalline rocks (original volume: 1010 m3). The mass movement comprises migmatites, leucogranites, orthogneisses and paragneisses (Weidinger et al. 2014). During mass-wasti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::383932a018138ef30fc531c29c163e45
https://doi.org/10.5194/egusphere-egu21-8442
https://doi.org/10.5194/egusphere-egu21-8442
Autor:
Diethard Sanders, Marc Ostermann, Jürgen Konzett, Bastian Joachim-Mrosko, Peter Tropper, Julian Lanthaler
The P-T conditions in extremely-rapid gravity-driven rockslides are difficult to constrain from the descended rock mass itself. Here, we report mineralogical observations from the Koefels rockslide and their interpretation. The Koefels event – happ
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cc630b1c9df2c7855e6111a077dd3a0f
https://doi.org/10.5194/egusphere-egu2020-4831
https://doi.org/10.5194/egusphere-egu2020-4831
Publikováno v:
Sedimentary Geology. 373:77-97
In studies of neotectonism, alluvial-fan and talus deposits commonly are used as deformation markers, but rarely are studied themselves and in relation to adjacent faults. Herein we report on the facies, diagenesis and deformation of a talus successi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::22bc05a0f6b66b93fa5b3d883d0ae1fa
https://doi.org/10.1016/j.sedgeo.2018.05.013
https://doi.org/10.1016/j.sedgeo.2018.05.013
Publikováno v:
Geomorphology. 301:39-52
Aeolian deposits record palaeoenvironmental conditions and may coin soil properties. Whereas periglacial loess is extensively investigated for ~ 200 years, the study of the intramontane wind-blown deposits of the Alps has just stuttered along. Herein
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ca580f742b4e60417fd145381672d982
https://doi.org/10.1016/j.geomorph.2017.10.025
https://doi.org/10.1016/j.geomorph.2017.10.025