Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Vaibhav Vijay Ingale"'
Autor:
Pierre-Yves Raumer, Sara Bazin, Dorian Cazau, Vaibhav Vijay Ingale, Jean-Yves Royer, Aude Lavayssière
Publikováno v:
Seismica, Vol 3, Iss 2 (2024)
Passive hydroacoustic studies have underscored the efficiency and relevance of deploying autonomous hydrophones for the surveillance of underwater geophony. In particular, monitoring networks have been deployed for detecting SOFAR-propagating hydroac
Externí odkaz:
https://doaj.org/article/bc741ade5dd24d8db25d5ba4f7134866
Hydroacoustic Observations of Two Contrasted Seismic Swarms along the Southwest Indian Ridge in 2018
Publikováno v:
Geosciences, Vol 11, Iss 6, p 225 (2021)
In 2018, two earthquake swarms occurred along spreading ridge segments of the ultra-slow Southwest Indian Ridge (SWIR). The first swarm was located at the spreading-ridge intersection with the Novara Fracture Zone, comprising 231 events (ISC catalogu
Externí odkaz:
https://doaj.org/article/242d14c8f0304048bc49192fa9da633f
Autor:
Pierre-Yves Raumer, Sara Bazin, Dorian Cazau, Vaibhav Vijay Ingale, Aude Lavayssière, Jean-Yves Royer
Hydrophones arrays have proven to be an efficient and affordable method to monitor underwater soundscape, in particular magmatic and tectonic events. Indeed, thanks to the sound fixing and ranging (SOFAR) channel in the ocean, acoustic waves undergo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ff5f329db3a0b5c33dd113ce26e2c676
https://doi.org/10.5194/egusphere-egu23-7028
https://doi.org/10.5194/egusphere-egu23-7028
Publikováno v:
Bulletin of the Seismological Society of America.
Hydroacoustic monitoring has become particularly efficient for studying the low-magnitude seismicity occurring at mid-ocean ridges. In 2016–2017, a seismic swarm occurred near the Melville transform fault of the ultraslow-spreading Southwest Indian
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8e8970a7cca14bfc0fe76c7d806dd82d
https://doi.org/10.1785/0120220213
https://doi.org/10.1785/0120220213
Seismic clusters of volcanic and tectonic events along mid-oceanic ridges are inherent to seafloor spreading. Due to the rapid attenuation of seismic waves in the solid Earth, land-based seismic networks lack the low-level seismicity associated with
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::88ff903e60ffc67fea15dff75df543ff
https://doi.org/10.5194/egusphere-egu22-462
https://doi.org/10.5194/egusphere-egu22-462
Hydroacoustic observations of Two Contrasted Seismic Swarms along the Southwest Indian Ridge in 2018
In 2018, two earthquake swarms occurred along segments of the ultra-slow Southwest Indian Ridge (spreading rate: 14-15 mm/a). The first swarm is located at the spreading-ridge intersection with the Atlantis Fracture Zone and comprises 9 Mw > 5.0 even
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bd51dcf1e4cb7c0559102965ead1ab04
https://doi.org/10.5194/egusphere-egu21-5131
https://doi.org/10.5194/egusphere-egu21-5131
Hydroacoustic observations of two contrasted seismic swarms along the Southwest Indian Ridge in 2018
Publikováno v:
Geosciences
Geosciences, MDPI, 2021, 11 (6), pp.225. ⟨10.3390/geosciences11060225⟩
Geosciences, Vol 11, Iss 225, p 225 (2021)
Geosciences (2076-3263) (MDPI AG), 2021-06, Vol. 11, N. 6, P. 225 (18p.)
Volume 11
Issue 6
Geosciences, MDPI, 2021, 11 (6), pp.225. ⟨10.3390/geosciences11060225⟩
Geosciences, Vol 11, Iss 225, p 225 (2021)
Geosciences (2076-3263) (MDPI AG), 2021-06, Vol. 11, N. 6, P. 225 (18p.)
Volume 11
Issue 6
International audience; In 2018, two earthquake swarms occurred along spreading ridge segments of the ultra-slow Southwest Indian Ridge (SWIR). The first swarm was located at the spreading-ridge intersection with the Novara Fracture Zone, comprising
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5dceb80eb9bb0f65c090605650559bb1
https://hal.univ-brest.fr/hal-03319875/document
https://hal.univ-brest.fr/hal-03319875/document