Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Juan Martin de Blas"'
Publikováno v:
Scientific Reports, Vol 14, Iss 1, Pp 1-18 (2024)
Abstract Tectonic plate motions drive the earthquake cycle, as they result in the slow accrual and sudden release of energy along plate boundaries. Steadiness of plate motions over the earthquake cycle is a central tenet of the plate tectonics theory
Externí odkaz:
https://doaj.org/article/bb259ae1cebd4fe591b29764fe77d5bd
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 25, Iss 2, Pp n/a-n/a (2024)
Abstract Tectonic plate motions are a prime constraint on lithosphere dynamics and on the torques acting upon plates. Researchers typically test hypotheses on the controlling torques via forward computer models, which allow accepting or rejecting hyp
Externí odkaz:
https://doaj.org/article/18b8e8d740744811aac1b1d9f54a1006
Publikováno v:
Scientific Reports, Vol 13, Iss 1, Pp 1-16 (2023)
Abstract Over million years, convergence between the Nazca and South America tectonic plates results in Andean orogeny. Over decades/centuries, it fuels the earthquake cycle of the Andean megathrust. It is well recognised that, over the geologically-
Externí odkaz:
https://doaj.org/article/0f11eb3045304d1991a75e09feaf3053
Publikováno v:
Scientific Reports, Vol 13, Iss 1, Pp 1-1 (2023)
Externí odkaz:
https://doaj.org/article/1bb81e4455fc4f7385c3c6b8540b29f9
Contemporary rigid motions of tectonic plates, which are inferred from geodetic data collected over several years, are commonly assumed to remain steady over the earthquake cycle. Such a tenet is predicated on the notion that stresses associated with
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::04881a8e4665a8e4a9394bbfc0fdac4c
https://doi.org/10.5194/egusphere-egu22-4483
https://doi.org/10.5194/egusphere-egu22-4483
In the current plate tectonics paradigm, relative plate motions remain unperturbed by temporal stress changes occurring during the seismic cycle, whereby the stress slowly built up along tectonic plate boundaries is suddenly released by rapid fault s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::92a746080218899a27bcc439d2939b1a
https://doi.org/10.5194/egusphere-egu22-4587
https://doi.org/10.5194/egusphere-egu22-4587
It is typically assumed that the relative plate motions are not affected by temporal stress changes occurring during the seismic cycle, which comprises a phase of slow buildup of stress (interseismic phase) followed by a phase of sudden release of st
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3909136ead5156d4168e444f0e106585
https://doi.org/10.5194/egusphere-egu22-4642
https://doi.org/10.5194/egusphere-egu22-4642
Publikováno v:
Iaffaldano, G, Martin de Blas, J & Í Dali Udbø, B 2022, ' Decadal change of the Apulia microplate motion preceding the M W 6.4, 26 November 2019 Durrës (Albania) earthquake ', Earth and Planetary Science Letters, vol. 584, 117505 . https://doi.org/10.1016/j.epsl.2022.117505
It is commonly assumed that the motions of tectonic plates remain steady over the earthquake cycle. This assumption is based on the notion that stresses associated with the cycle may not be sufficient to overcome the asthenosphere viscous resistance
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::42d3f8638318687098f87b111bd8f8a6
https://curis.ku.dk/ws/files/316684100/Decadal_change_of_the_Apulia_microplate_motion_preceding.pdf
https://curis.ku.dk/ws/files/316684100/Decadal_change_of_the_Apulia_microplate_motion_preceding.pdf