Zobrazeno 1 - 10
of 50
pro vyhledávání: '"Francesca Meneghini"'
Autor:
Genevieve L. Coffey, Heather M. Savage, Pratigya J. Polissar, Francesca Meneghini, Matt J. Ikari, Åke Fagereng, Julia K. Morgan, Maomao Wang
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 22, Iss 8, Pp n/a-n/a (2021)
Abstract The Hikurangi subduction zone is capable of producing moderate to large earthquakes as well as regularly repeating slow slip events. However, it is unclear what structures host these different slip styles along the margin. Here we address wh
Externí odkaz:
https://doaj.org/article/9b7dd37af7d344459aa0f502eed9bd57
Autor:
Heather M. Savage, Srisharan Shreedharan, Åke Fagereng, Julia K. Morgan, Francesca Meneghini, Maomao Wang, David D. McNamara, Laura M. Wallace, Demian M. Saffer, Philip M. Barnes, Katerina E. Petronotis, Leah J. LeVay
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 22, Iss 8, Pp n/a-n/a (2021)
Abstract Quantifying fault damage zones provides a window into stress distribution and rheology around faults. International Ocean Discovery Program (IODP) Expeditions 372/375 drilled an active thrust splay fault within the Hikurangi subduction margi
Externí odkaz:
https://doaj.org/article/c8da92d3ec1a4728b7b4ef24d6f257c8
Autor:
Julia K. Morgan, Evan A. Solomon, Ake Fagereng, Heather M. Savage, Maomao Wang, Francesca Meneghini, Philip M. Barnes, Rebecca E. Bell, Melodie E. French, Nathan L. Bangs, Hiroko Kitajima, Demian M. Saffer, Laura M. Wallace
Publikováno v:
Earth and Planetary Science Letters. 593:117651
IODP Site U1518, drilled during IODP Expeditions 372 and 375, penetrated a large-offset (∼6 km) thrust, the Pāpaku fault, rising from a megathrust that hosts recurring slow slip events along the Hikurangi margin. Although drilling intersected the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d9d735850e546fb9df19865e4dea8fc2
https://doi.org/10.1016/j.epsl.2022.117651
https://doi.org/10.1016/j.epsl.2022.117651
Publikováno v:
Episodes. 42:107-118
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3a932601ca707793dcdd8c0cdd19d018
https://doi.org/10.18814/epiiugs/2019/019009
https://doi.org/10.18814/epiiugs/2019/019009
The geological properties of the subduction interface, such as stable metamorphic assemblages and the rheology of shear zone rocks, change with depth. Studies based on seismic and geodetic observations suggest that these changes can be accompanied by
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c5599d2cca51ef2c0fcad2e2830ba97b
https://doi.org/10.5194/egusphere-egu21-10990
https://doi.org/10.5194/egusphere-egu21-10990
Publikováno v:
Nature Communications
Nature Communications, Vol 12, Iss 1, Pp 1-8 (2021)
Nature Communications, Vol 12, Iss 1, Pp 1-8 (2021)
In subduction zones, seismic slip at shallow crustal depths can lead to the generation of tsunamis. Large slip displacements during tsunamogenic earthquakes are attributed to the low coseismic shear strength of the fluid-saturated and non-lithified c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b4b5ba4e5c74c27eea5cbd9e6f0c3da9
https://doi.org/10.5194/egusphere-egu21-8241
https://doi.org/10.5194/egusphere-egu21-8241
Autor:
Demian M. Saffer, Maomao Wang, Katerina Petronotis, Srisharan Shreedharan, Julia K. Morgan, Leah J. LeVay, Francesca Meneghini, David D. McNamara, Heather M. Savage, Laura M. Wallace, Philip M. Barnes, Ake Fagereng
Publikováno v:
Geochemistry, Geophysics, Geosystems
Quantifying fault damage zones provides a window into stress distribution and rheology around faults. International Ocean Discovery Program (IODP) Expeditions 372/375 drilled an active thrust splay fault within the Hikurangi subduction margin. The fa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::48a713b581b3039cc3000db89a0e802c
http://hdl.handle.net/11568/1115838
http://hdl.handle.net/11568/1115838
Autor:
Maomao Wang, Harold Leah, Rebecca E. Bell, Ake Fagereng, Julia K. Morgan, Matt J. Ikari, Francesca Meneghini, Heather M. Savage
Publikováno v:
Tectonics
Calcareous‐pelagic input sediments are present at several subduction zones and deform differently to their siliciclastic counterparts. We investigate deformation in calcareous‐pelagic sediments drilled ~20 km seaward of the Hikurangi megathrust t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bae1fbbb59e3259b927dc3ff7c3a81a5
http://hdl.handle.net/10044/1/82946
http://hdl.handle.net/10044/1/82946
Publikováno v:
Tectonics. 36:2227-2249
The Meso-Cenozoic alpine belts of the Mediterranean area are characterized by complex architectures, result of a complex subduction and collision evolution that preserve also a legacy of the rifting-related configuration of the continental margins. T
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::78c1173e0690ea83f99431b682f44ce3
https://doi.org/10.1002/2017tc004627
https://doi.org/10.1002/2017tc004627
Publikováno v:
Neuroepidemiology ISBN: 9780429277276
Myasthenia gravis (MG) is a neuromuscular junction disorder in which the basic pathophysiologic mechanism is binding of the postsynaptic acetylcholine receptors by abnormally produced antibodies, with resultant blockage of muscle response. This chapt
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7ed269b4379dd7ce9a50937b194d7b9c
https://doi.org/10.1201/9780429277276-15
https://doi.org/10.1201/9780429277276-15