Zobrazeno 1 - 10
of 26
pro vyhledávání: '"Carlos Villafuerte"'
Publikováno v:
American Journal of Perinatology Reports, Vol 14, Iss 03, Pp e224-e227 (2024)
Background TRAP sequence occurs in monochorionic pregnancies consisting of one normal fetus and a non-viable fetus. The pump twin has an increased risk of developing high-output cardiac failure.
Externí odkaz:
https://doaj.org/article/83598a5d904549d2af7e1287c7528c5d
Autor:
Aron Mirwald, Víctor M. Cruz‐Atienza, John Díaz‐Mojica, Arturo Iglesias, Shri K. Singh, Carlos Villafuerte, Josué Tago
Publikováno v:
Geophysical Research Letters, Vol 46, Iss 4, Pp 2054-2064 (2019)
Abstract We investigate dynamic source parameters of the Mw7.1 Puebla‐Morelos intermediate‐depth earthquake (h = 57 km) of 19 September 2017, which devastated Mexico City. Our simple, elliptical source model, coupled with a new Particle Swarm Opt
Externí odkaz:
https://doaj.org/article/6c2a6492f8b3437c8fbfddfb2d54c769
Publikováno v:
Nature Communications, Vol 9, Iss 1, Pp 1-13 (2018)
Rapid tremor migration in subduction zones has been associated with aseismic, shear strain at the plate interface. Here, the authors develop a physical model that shows that pore-pressure waves at the plate interface are likely to generate secondary
Externí odkaz:
https://doaj.org/article/757a5ff552aa41489c0fe4b42f027bf5
The elastic medium that hosts several, multi-scale, faults could be regarded as an energy reservoir that is charged by the far field stress rate and discharged by friction dissipation during earthquake slips on the faults. In this study, we carefully
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::86e679ad9e32758a77c79b3bd8a2c2a7
https://doi.org/10.5194/egusphere-egu23-3982
https://doi.org/10.5194/egusphere-egu23-3982
Over the last decades, new observations of complex slip dynamics have emerged. We now observe a continuum of transients energy release happening on fault systems, such as slow slip events, LFEs and tremors. Present quasi-dynamic numerical models are
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::56399921caa424900333fbd92447ecc7
https://doi.org/10.5194/egusphere-egu23-7998
https://doi.org/10.5194/egusphere-egu23-7998
In addition to regular earthquakes, observations of spatiotemporally complex slip events have multiplied over the last decades. These slip events range along different time scales: from creep , slow slip events to LFEs and tremors. At present, these
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::093bb2fd5f2037d44277078d2909ad39
https://doi.org/10.5194/egusphere-egu23-16290
https://doi.org/10.5194/egusphere-egu23-16290
Major earthquake ruptures occur predominantly in thrust faults producing devastating events and tsunamis such as the 2011 Mw 9.0 Tohoku earthquake, the 2004 Mw 9.2 Sumatra earthquake and the 1999 Mw 7.7 Chi-Chi earthquake. Understanding the mechanics
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9e6b88b690130b2d6b42e29b6d5a4b6e
https://doi.org/10.5194/egusphere-egu23-7849
https://doi.org/10.5194/egusphere-egu23-7849
Publikováno v:
Salud Pública de México, Vol 60, Iss 3, may-jun, Pp 373-374 (2018)
[Not available]
Externí odkaz:
https://doaj.org/article/e8af3134a5c54c9cac1421313f675baa
Autor:
Yoshihiro Ito, Vladimir Kostoglodov, Takuya Nishimura, Josué Tago, Jorge Real, Víctor M. Cruz-Atienza, Carlos Villafuerte
Publikováno v:
Geophysical Journal International. 226:1187-1205
SUMMARYTo shed light on the prevalently slow, aseismic slip interaction between tectonic plates, we developed a new static slip inversion strategy, the ELADIN (ELastostatic ADjoint INversion) method, that uses the adjoint elastostatic equations to co
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::36b09671c7528cc91cb2b27204104b6f
https://doi.org/10.1093/gji/ggab165
https://doi.org/10.1093/gji/ggab165
Thrust faults are commonly known to produce significant amounts of slip, damage and ground acceleration, especially close to the free surface. The effect of the free surface on faulting has always been a standing issue in theoretical mechanics. While
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7cff52d59ad6c251cde68cee22a8e32e
https://doi.org/10.5194/egusphere-egu22-12223
https://doi.org/10.5194/egusphere-egu22-12223