Zobrazeno 1 - 10
of 22
pro vyhledávání: '"Tore J. Kvalstad"'
Autor:
Tore J. Kvalstad, Siren Knudsen, Haflidi Haflidason, Heidi Kjennbakken, Muhammad Adeel Mazhar, Maarten Vanneste, Søren Holm, Carl Fredrik Forsberg, Samson Abate Degago, Finn Løvholt, Brian Carlton
Publikováno v:
Geological Society, London, Special Publications. 477:549-566
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ba24883028e0e7d35453dcce555b8d74
https://doi.org/10.1144/sp477.39
https://doi.org/10.1144/sp477.39
Autor:
Maarten Vanneste, Jan Sverre Laberg, Haflidi Haflidason, Nicole J. Baeten, Tore O. Vorren, Carl Fredrik Forsberg, Tore J. Kvalstad, Matthias Forwick
Publikováno v:
Journal of Geophysical Research: Earth Surface. 119:2335-2360
Submarine landslides are often characterized by a basal surface of rupture parallel to the stratigraphy, in which downslope movement is initiated. However, little is known about the sedimentology and physical properties of the sediments within these
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4c349a0b13bcd58ecb85616e34cef81b
https://doi.org/10.1002/2013jf003068
https://doi.org/10.1002/2013jf003068
Autor:
Haflidi Haflidason, Jo Brendryen, Maarten Vanneste, Farrokh Nadim, Jean-Sébastien L'Heureux, Shyam Chand, Oddvar Longva, Carl Fredrik Forsberg, Tore J. Kvalstad, Leif Rise
Publikováno v:
Marine Geology. 346:192-207
Several relatively small and spatially-isolated landslides with low mobility characterize the geomorphology of the upper continental slope off the Vesteralen islands. Here, we present results from a multidisciplinary study that integrates swath bathy
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9577d8024ed197f8749593e6aa9cb7a3
https://doi.org/10.1016/j.margeo.2013.09.009
https://doi.org/10.1016/j.margeo.2013.09.009
Autor:
Maarten Vanneste, Carl Fredrik Forsberg, Jan Sverre Laberg, Tore J. Kvalstad, M.K. Ivanov, Nicole J. Baeten, Tore O. Vorren, Matthias Forwick
Publikováno v:
Geomorphology. 187:122-134
Little attention has been paid to smaller-scale mass movements on continental slopes, even though they occur much more frequently than their large-scale counterparts. Swath bathymetry, side-scan sonar, sub-bottom profiler and seismic data from the co
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9d6225f57ea0a5d197129889148e413b
https://doi.org/10.1016/j.geomorph.2013.01.008
https://doi.org/10.1016/j.geomorph.2013.01.008
Publikováno v:
Marine and Petroleum Geology. 22:311-318
The Ormen Lange gas field is located within the slide scar of the enormous Storegga Slide that took place about 8200 years ago. There are strong indications that the Storegga slide generated a tsunami wave hitting the coastlines of Norway, Scotland a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::55a67158a1cec77fafdc6d4076caaee3
https://doi.org/10.1016/j.marpetgeo.2004.10.022
https://doi.org/10.1016/j.marpetgeo.2004.10.022
Publikováno v:
Marine and Petroleum Geology. 22:299-310
The Ormen Lange gas field is located in 850–1100 m water depth in the slide scar of the enormous Storegga Slide. This slide occurred about 8200 years ago and left steep and high scarps above and below the planned field development area. Today's sta
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4d98eee9a01a96b5fa6ede7e1996534f
https://doi.org/10.1016/j.marpetgeo.2004.10.021
https://doi.org/10.1016/j.marpetgeo.2004.10.021
Publikováno v:
Marine and Petroleum Geology. 22:245-256
The Storegga slide occurred about 8200 years ago. The enormous slide was released in an area where the average slope inclination is in the order of 0.6–0.7°. Slide mechanisms and possible triggering sources that can cause large scale slide events
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1399eabf611bdd936e0ce12f31a7a6cf
https://doi.org/10.1016/j.marpetgeo.2004.10.019
https://doi.org/10.1016/j.marpetgeo.2004.10.019
Publikováno v:
Marine and Petroleum Geology. 22:11-19
The Storegga Slide occurred 8200 years ago and was the last megaslide in this region where similar slides have occurred with intervals of approximately 100 ky since the onset of continental shelf glaciations at 0.5 Ma. A geological model for the Plio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a7b658b551f9dd65ae2130b25b199bf7
https://doi.org/10.1016/j.marpetgeo.2004.12.003
https://doi.org/10.1016/j.marpetgeo.2004.12.003
Autor:
Maarten Vanneste, Moerz Tobias, Jean-Sébastien L'Heureux, Oddvar Longva, Isabelle Lecomte, Mark E. Vardy, Haflidi Haflidason, Carl Fredrik Forsberg, Jo Brendryen, J.M. Strout, Alois Steiner, Stefan Kreiter, Eugene Morgan, Tore J. Kvalstad, Achim J Kopf
Publikováno v:
All Days.
Abstract Sørfjord outside the village of Finneidfjord has a history of landsliding throughout the Holocene. The 1996 landslide -the focus of this study - has many characteristics typical of submarine landslides (well-developed slip plane, outrunner
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::15f9949eb021e5d5ddcd3681b3a5186d
https://doi.org/10.4043/23967-ms
https://doi.org/10.4043/23967-ms
Autor:
Sylfest Glimsdal, Carl Fredrik Forsberg, Farrokh Nadim, Maarten Vanneste, Dieter Issler, Finn Løvholt, Carl B. Harbitz, Tore J. Kvalstad
Publikováno v:
Landslide Science and Practice ISBN: 9783642314261
The threats posed by submarine landslides to human civilization are the disappearance of valuable land near the shoreline, the destruction of seafloor installations like cables, pipelines or oil wells, and – most importantly – the devastation of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1d254e764536049e938d7d2adcfdba6b
https://doi.org/10.1007/978-3-642-31427-8_1
https://doi.org/10.1007/978-3-642-31427-8_1
