Zobrazeno 1 - 10
of 16
pro vyhledávání: '"Michael Schnellmann"'
Autor:
Tobias Diehl, Herfried Madritsch, Michael Schnellmann, Thomas Spillmann, Elmar Brockmann, Stefan Wiemer
Publikováno v:
Tectonophysics, 846
This study presents a seismotectonic analysis of the Miocene-aged Hegau-Bodensee Graben, a major tectonic element in the northern foreland of the European Central Alps. The graben is characterized by comparatively low strain rates and low-to-moderate
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::287f679adf725fc8cec55fa29c7a885f
Autor:
Tobias Diehl, Herfried Madritsch, Michael Schnellmann, Thomas Spillmann, Elmar Brockmann, Stefan Wiemer
This study presents a seismotectonic analysis of the Miocene-aged Bodensee-Hegau Graben, a major tectonic element in the northern foreland of the European Central Alps. The graben is characterized by comparatively low strain rates and low to moderate
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aca30a3ddcb114c62ef8a77e3ae30087
https://doi.org/10.5194/egusphere-egu22-6018
https://doi.org/10.5194/egusphere-egu22-6018
Autor:
Michael Schnellmann, Tim Vietor
The site selection process for the deep geological repositories in Switzerland is in its final phase. All three remaining sites fulfil the requirements of the repositories for low level waste (LLW) as well as for high level waste (HLW) and spent fuel
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ac10cd393f64d72527f7acd581551fb6
https://sand.copernicus.org/articles/1/51/2021/
https://sand.copernicus.org/articles/1/51/2021/
Publikováno v:
Journal of Geophysical Research: Earth Surface. 122:2196-2222
Landscape evolution is a product of the forces that drive geomorphic processes (e.g., tectonics and climate) and the resistance to those processes. The underlying lithology and structural setting in many landscapes set the resistance to erosion. This
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cd304f2e3412819eba78531acf441b00
https://doi.org/10.1002/2016jf004101
https://doi.org/10.1002/2016jf004101
Publikováno v:
Journal of Geophysical Research: Earth Surface. 118:1060-1084
[1] Landscape evolution is controlled by the development and organization of drainage basins. As a landscape evolves, drainage reorganization events can occur via river capture or piracy, whereby one river basin grows at the expense of another. The r
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::303c592935b65aeb6c10a4d1abaf7828
https://doi.org/10.1002/jgrf.20056
https://doi.org/10.1002/jgrf.20056
Publikováno v:
SEDIMENTOLOGY
Central Switzerland lies tectonically in an intraplate area and recurrence rates of strong earthquakes exceed the time span covered by historic chronicles. However, many lakes are present in the area that act as natural seismographs: their continuous
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::66e19a061ed442f93885e23061ec6578
https://doi.org/10.1111/sed.12003
https://doi.org/10.1111/sed.12003
Autor:
Flavio S. Anselmetti, Juan Pablo Corella, Daniel Ariztegui, Blas L. Valero-Garcés, Pilar Mata, M. Rico, Ana Moreno, Michael Schnellmann, Mario Morellón
Publikováno v:
Sedimentology, Vol. 56, No 5 (2009) pp. 1505-1534
Digital.CSIC. Repositorio Institucional del CSIC
instname
Digital.CSIC. Repositorio Institucional del CSIC
instname
30 páginas, 10 figuras, 4 tablas.-- El PDF del artículo es su versión post-print.
Lake Estanya is a small (19 ha), freshwater to brackish, monomictic lake formed by the coalescence of two karstic sinkholes with maximum water depths of 12 and
Lake Estanya is a small (19 ha), freshwater to brackish, monomictic lake formed by the coalescence of two karstic sinkholes with maximum water depths of 12 and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::058f25345b349cfa001f674e58938034
https://doi.org/10.1111/j.1365-3091.2008.01044.x
https://doi.org/10.1111/j.1365-3091.2008.01044.x
Publikováno v:
Eclogae Geologicae Helvetiae, 99 (3)
Eclogae Geologicae Helvetiae, 99 (3)
ISSN:0012-9402
ISSN:1420-9128
ISSN:0012-9402
ISSN:1420-9128
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8bfcf861d71a6bdb8f207d80d2962475
https://doi.org/10.1007/s00015-006-1196-7
https://doi.org/10.1007/s00015-006-1196-7
Publikováno v:
Tectonophysics. 400:153-177
A multiarchive approach has been applied to the investigation of the late Pleistocene and Holocene record of strong earthquakes in Switzerland. The geological archives used for this study include active faults, lake deposits, slope instabilities, and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::372c760c6f65d1d142d61d5968b28f6b
https://doi.org/10.1016/j.tecto.2005.03.001
https://doi.org/10.1016/j.tecto.2005.03.001
Publikováno v:
Sedimentology. 52:271-289
High-resolution seismic imaging and piston coring in Lake Lucerne, Switzerland, have revealed surprising deformation structures in flat-lying, unconsolidated sediment at the foot of subaqueous slopes. These deformation structures appear beneath wedge
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::20b52d2d90111e758bee77f4bc9808e0
https://doi.org/10.1111/j.1365-3091.2004.00694.x
https://doi.org/10.1111/j.1365-3091.2004.00694.x