Zobrazeno 1 - 10
of 17
pro vyhledávání: '"Bernhard Schuck"'
Autor:
Jirapat Charoensawan, Ludmila Adam, Michael Ofman, Virginia Toy, Jonathan Simpson, Xin Zhong, Bernhard Schuck
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
P-wave anisotropy is significant in the mylonitic Alpine Fault shear zone. Mineral- and texture-induced anisotropy are dominant in these rocks but further complicated by the presence of fractures. Electron back-scattered diffraction and synchrotron X
Externí odkaz:
https://doaj.org/article/065ac0e07bda466ba296277b2984f647
The tectonophysical paradigm that earthquake ruptures should not start, or easily propagate into, the shallowest few kilometers of Earth’s crust makes it difficult to understand why damaging surface displacements have occurred during historic event
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::674598fa092e167b195374d76dde352c
https://doi.org/10.5194/egusphere-egu21-8627
https://doi.org/10.5194/egusphere-egu21-8627
Autor:
Steffen Abe, Virginia Toy, Till Sachau, Philipp Seelos, Sebastian G. Mutz, Selina S. Fenske, Martina Kirilova, Hagen Deckert, Paul D. Bons, Simon J. Buckley, Julian Owin, Conor Lewis, Bernhard Schuck
In September 2020, the Corona crisis offered us an opportunity to develop and test a blended real and virtual interdisciplinary field mapping class, as well as revealing the need for, and stimulating development of new web-based tools for structural
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dbf8d31eb605888d182156e9673c4fca
https://doi.org/10.5194/egusphere-egu21-3581
https://doi.org/10.5194/egusphere-egu21-3581
Autor:
Tilo Kneuker, Bernhard Schuck
Publikováno v:
Safety of Nuclear Waste Disposal. 1:47-48
Deep geological formations are considered for safe long-term disposal of high-level radioactive waste. Such a repository would be requested to prevent radionuclides from entering the biosphere for a period of 1 million years (StandAG, 2017). Conseque
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::395b0b546f53b21304726b1d10fcc4c2
https://doi.org/10.5194/sand-1-47-2021
https://doi.org/10.5194/sand-1-47-2021
Autor:
Xin Zhong, Michael Ofman, Jirapat Charoensawan, Virginia Toy, Bernhard Schuck, Jonathan Simpson, Ludmila Adam
Publikováno v:
Frontiers in Earth Science
Frontiers in Earth Science, Vol 9 (2021)
Frontiers in Earth Science, Vol 9 (2021)
P-wave anisotropy is significant in the mylonitic Alpine Fault shear zone. Mineral- and texture-induced anisotropy are dominant in these rocks but further complicated by the presence of fractures. Electron back-scattered diffraction and synchrotron X
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::40908f6afefdbbeefd73b8e8dc65bbd8
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5007503
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5007503
Autor:
Nicolas C. Barth, Risa Matsumura, Mark Stirling, Caroline Orchiston, Virginia Toy, Bernhard Schuck
There is currently around a 30% probability New Zealand’s Alpine Fault will accommodate another M~8 earthquake in the next 50 years. The fault passes through Franz Josef Glacier town, a popular tourist destination attracting up to 6,000 visitors pe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::af9d11aa26c2eeb8e29065538bf09ac4
https://doi.org/10.5194/egusphere-egu2020-5316
https://doi.org/10.5194/egusphere-egu2020-5316
Publikováno v:
Solid Earth
New Zealand's Alpine Fault is a large, plate-bounding strike-slip fault, that ruptures in large (MW > 8) earthquakes. Its hazard potential is linked to its geometrical properties. We conducted field and laboratory analyses of fault rocks to elucidate
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::566777c2ace3d192fdfebd6ac50c6aa4
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5000142_1/component/file_5000171/5000142.pdf
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5000142_1/component/file_5000171/5000142.pdf
Publikováno v:
Journal of Structural Geology
The Alpine Fault is capable of generating large (MW > 8) earthquakes and is the main geohazard on South Island, NZ, and late in its 250–291-year seismic cycle. To minimize its hazard potential, it is indispensable to identify and understand the pro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c06f0c3b793b705ada472eb4b126c08d
https://doi.org/10.1016/j.jsg.2018.03.001
https://doi.org/10.1016/j.jsg.2018.03.001