Zobrazeno 1 - 10
of 11
pro vyhledávání: '"Gauvain Wiemer"'
Autor:
Robert Kopte, Marius Becker, Tim Fischer, Peter Brandt, Gerd Krahmann, Maximilian Betz, Claas Faber, Christian Winter, Johannes Karstensen, Gauvain Wiemer
Publikováno v:
Frontiers in Marine Science, Vol 11 (2024)
This paper presents the open-source Python software OSADCP developed for the processing of vessel-mounted Acoustic Doppler Current Profiler (VMADCP) data. At this stage, the toolbox is designed for processing VMADCP measurements from open-ocean appli
Externí odkaz:
https://doaj.org/article/970922691d6240adb42bbcd8b817e909
Publikováno v:
Geological Society, London, Special Publications. 500:129-146
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::210a3edea499b37f9f815d14575e8c08
https://doi.org/10.1144/sp500-2019-155
https://doi.org/10.1144/sp500-2019-155
Autor:
Irka Hajdas, Mario Pino, M. De Batist, Daniel Melnick, Roberto Urrutia, Jasper Moernaut, Thomas Vandorpe, Katrien Heirman, Gauvain Wiemer, Ariana Molenaar, M. Van Daele
Publikováno v:
Sedimentary Geology. 381:84-105
Subaqueous landslides are common features at active and passive ocean margins, in fjords and lakes. They can develop on very gentle slope gradients (
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e01c0b82ea13500c30ddbc231fad3f42
https://doi.org/10.1016/j.sedgeo.2019.01.002
https://doi.org/10.1016/j.sedgeo.2019.01.002
Autor:
Gauvain Wiemer, Ting-Wei Wu, Michael Strasser, Achim J Kopf, Ariana Molenaar, Jasper Moernaut
Earthquakes are a main trigger of subaqueous landslides and surficial sediment remobilization at ocean margins and lake basins. If the earthquake loading is insufficient to lead to sediment failure, the subsequent dewatering and inherent compaction m
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::28b9a14c5eb284021d6be06b1af1e182
https://doi.org/10.5194/egusphere-egu2020-2578
https://doi.org/10.5194/egusphere-egu2020-2578
Publikováno v:
Marine Geology. 385:173-184
Marine diatomaceous sediments are common along the polar belts and equator, but very little is known about their effect on sediment geotechnical properties and slope stability. Consolidation state analysis is frequently applied to derive past maximum
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c827e5d00070fd1e73cb24db2a918d7f
https://doi.org/10.1016/j.margeo.2017.01.006
https://doi.org/10.1016/j.margeo.2017.01.006
Autor:
Gauvain Wiemer, Achim J Kopf
Publikováno v:
Geochemistry, Geophysics, Geosystems. 18:333-345
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7ac6cfaa87cbd15b0a668ac5b275bca1
https://doi.org/10.1002/2016gc006568
https://doi.org/10.1002/2016gc006568
Autor:
Marc De Batist, Gauvain Wiemer, Michael Strasser, Anna Reusch, Achim J Kopf, Roberto Urrutia, Nina Stark, Jasper Moernaut, Bruno Ladrón de Guevara
Publikováno v:
Marine Geology
Pore fluid pressure is a key parameter for subaquatic slope stability and has been put forward to explain the development of many submarine landslides especially when occurring on very gentle slopes or in areas with high sedimentation rate. Due to th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fdd63b27e5ebbcdad4f50dcec4b770e3
Autor:
Gauvain Wiemer, Achim J Kopf
Publikováno v:
Landslides. 14:223-232
Volcanic ash deposits have been proposed to potentially liquefy and act as preferential failure planes during submarine landslides along active margins. However, particle angularity and surface roughness of volcanic material significantly influence i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b936f1b92137c6e1cf2903c2c7dff2cf
https://doi.org/10.1007/s10346-016-0706-6
https://doi.org/10.1007/s10346-016-0706-6
Autor:
Achim J Kopf, Gauvain Wiemer
Publikováno v:
Geo-Marine Letters. 35:305-314
Weathering of tephra results in increasing proportions of mechanically weak, authigenic clay minerals (smectite). This suggests that altered tephra represent inherent weak layers in slope sediment sequences, and these may facilitate slope failure in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::98221404c639d39845381c65f55e535b
https://doi.org/10.1007/s00367-015-0408-4
https://doi.org/10.1007/s00367-015-0408-4
Autor:
Nina Stark, Mario Pino, Michael Strasser, Achim J Kopf, Gauvain Wiemer, Marc De Batist, Bruno Ladrón de Guevara, Philipp Kempf, Roberto Urrutia, Jasper Moernaut
Publikováno v:
International Journal of Earth Sciences
© 2015 Springer Verlag Berlin Heidelberg. Subaqueous slope failure mechanisms are still poorly understood partly because they are difficult to study due to the remote location of submarine landslides. Landslides in lakes are smaller in size and more
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0148acfce84006241a758a49117e87f8
https://doi.org/10.1007/s00531-015-1144-8
https://doi.org/10.1007/s00531-015-1144-8