Zobrazeno 1 - 10
of 13
pro vyhledávání: '"Arianne Petley-Ragan"'
Autor:
Luca Menegon, Arianne Petley-Ragan, Sarah Incel, Bjørn Jamtveit, Håkon Austrheim, Fernando Corfu, Kristina G. Dunkel, François Renard, Claire Aupart
Publikováno v:
Journal of Geophysical Research: Solid Earth
Rock rheology and density have first‐order effects on the lithosphere's response to plate tectonic forces at plate boundaries. Changes in these rock properties are controlled by metamorphic transformation processes that are critically dependent on
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b75d8381c94faf35bfc59bcf77616ba8
https://doi.org/10.1029/2018jb016461
https://doi.org/10.1029/2018jb016461
Autor:
Niels H. Andersen, Xin Zhong, Marcin Dabrowski, Sarah Incel, Bjørn Jamtveit, Arianne Petley-Ragan
Publikováno v:
Nature Geoscience
Earthquakes at lower crustal depths are common during continental collision. However, the coseismic weakening mechanisms required to propagate an earthquake at high pressures are poorly understood. Transient high-pressure fluids or melts have been pr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a7ec932b75683f99090362bf0f8b5db3
Autor:
Marcin Dabrowski, Arianne Petley-Ragan, Niels H. Andersen, Bjørn Jamtveit, Håkon Austrheim, Xin Zhong, Sarah Incel
Earthquakes are among the most catastrophic geological events that last only several to tens of seconds. During earthquakes, many processes may occur including rupturing, frictional sliding, pore fluid pressurization and occasionally frictional melti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::067ae9c380f871e0c097c72202e7f9bd
https://doi.org/10.5194/egusphere-egu2020-5204
https://doi.org/10.5194/egusphere-egu2020-5204
A significant number of studies in recent years have demonstrated that earthquakes in the lower crust are more abundant than previously thought. Specifically in continental collision zones, earthquakes are suggested to play a crucial role in permitti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::41d2bc3c321b8102d9bb3d3f52853cf4
https://doi.org/10.5194/egusphere-egu2020-8965
https://doi.org/10.5194/egusphere-egu2020-8965
Caledonian eclogite- and amphibolite-facies metamorphism of initially dry Proterozoic granulites in the Lindås Nappe of the Bergen Arcs, Western Norway, is driven by fluid infiltration along faults and shear zones. The granulites are also cut by num
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fbd19d077d55e79e7d7c00a6f982e32d
https://doi.org/10.5194/egusphere-egu2020-2154
https://doi.org/10.5194/egusphere-egu2020-2154
Autor:
Håkon Austrheim, Bjørn Jamtveit, Arianne Petley-Ragan, Benoit Ildefonse, Yehuda Ben-Zion, François Renard
Publikováno v:
Science Advances
Science Advances, American Association for the Advancement of Science (AAAS), 2019, 5 (7), pp.eaaw0913. ⟨10.1126/sciadv.aaw0913⟩
Science Advances, 2019, 5 (7), pp.eaaw0913. ⟨10.1126/sciadv.aaw0913⟩
'Science Advances ', vol: 5, pages: eaaw0913-1-eaaw0913-8 (2019)
Science Advances, American Association for the Advancement of Science (AAAS), 2019, 5 (7), pp.eaaw0913. ⟨10.1126/sciadv.aaw0913⟩
Science Advances, 2019, 5 (7), pp.eaaw0913. ⟨10.1126/sciadv.aaw0913⟩
'Science Advances ', vol: 5, pages: eaaw0913-1-eaaw0913-8 (2019)
A lower crustal earthquake is initiated by dynamic rupturing with fragmentation of wall rock that precedes frictional melting.
Earthquakes in the continental crust commonly occur in the upper 15 to 20 km. Recent studies demonstrate that earthqua
Earthquakes in the continental crust commonly occur in the upper 15 to 20 km. Recent studies demonstrate that earthqua
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::daca3aff808346a0f39132383364ed99
https://doi.org/10.1126/sciadv.aaw0913
https://doi.org/10.1126/sciadv.aaw0913
Publikováno v:
Journal of Metamorphic Geology. 34:85-101
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::009589def307ebcabf9f80c16178ca27
https://doi.org/10.1111/jmg.12172
https://doi.org/10.1111/jmg.12172