Zobrazeno 1 - 10
of 37
pro vyhledávání: '"P. E. Share"'
Publikováno v:
Journal of Geophysical Research: Solid Earth. 128
Autor:
Pierre Boué, Yifang Cheng, P. E. Share, Frank L. Vernon, Florent Brenguier, Chris Johnson, Aurélien Mordret, Yehuda Ben-Zion, Zefeng Li
Publikováno v:
Seismological Research Letters. 91:2862-2871
We propose a new automated procedure for using continuous seismic waveforms recorded by a dense array and its nearby regional stations for P-wave arrival identification, location, and magnitude estimation of small earthquakes. The method is illustrat
Autor:
Frank L. Vernon, P. E. Share, Thomas K. Rockwell, J Ramón Arrowsmith, Petr Tábořík, Petra Štěpančíková, Adam Wade, Yehuda Ben-Zion, Andrea Donnellan, Jakub Stemberk
Publikováno v:
Geophysical Journal International. 222:781-794
SUMMARYWe present results from complementary geological, topographic, seismic and electrical resistivity surveys at the Sagebrush Flat (SGB) site along the Clark fault (CF) strand of the San Jacinto fault zone trifurcation area southeast of Anza, Cal
Publikováno v:
Geophysical Journal International, vol 224, iss 2
SUMMARYWe image the internal structure of the San Jacinto fault zone (SJFZ) near Anza, California, with seismic data recorded by two dense arrays (RA and RR) from ∼42 000 local and ∼180 teleseismic events occurring between 2012 and 2017. The RA l
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6c17d4dd1261e754e0b995a430cfab1c
https://escholarship.org/uc/item/3637g12k
https://escholarship.org/uc/item/3637g12k
Autor:
Pierre Boué, Frank L. Vernon, Chris Johnson, P. E. Share, Florent Brenguier, Yehuda Ben-Zion, Aurélien Mordret
Laboratory experiments report that detectable seismic velocity changes should occur in the vicinity of fault zones prior to earthquakes. However, operating permanent active seismic sources to monitor natural faults at seismogenic depth has been nearl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8e8fa9c4f9f1f5c64b5975f2df512be1
https://doi.org/10.5194/egusphere-egu2020-5480
https://doi.org/10.5194/egusphere-egu2020-5480
Publikováno v:
Pure and Applied Geophysics. 176:1117-1143
We derive high-resolution P and S seismic velocities (VP and VS) within the South-Central Transverse Ranges section of the San Andreas Fault (SAF), using a new double-difference tomography algorithm incorporating both event-pair and station-pair diff
Publikováno v:
Pure and Applied Geophysics. 176:1169-1191
We image the San Jacinto fault zone at Blackburn Saddle using earthquake waveforms recorded by a ~ 2-km across-fault linear array with 108 three-component sensors separated by ~ 10–30 m. The length and spatiotemporal sampling of the array allow us
Publikováno v:
Geophysical Journal International. 213:98-114
We image the internal structure of the San Jacinto fault zone (SJFZ) in the trifurcation area southeast of Anza, California, with seismic records from dense linear and rectangular arrays. The examined data include recordings from more than 20 000 loc
Publikováno v:
Earth and Planetary Science Letters. 568:117004
We image seismic properties of the plate boundary through northern Baja California and southernmost California using a double-difference tomography and earthquake relocation algorithm that incorporates both event-pair and station-pair data. The data
Autor:
Frank L. Vernon, Eric Beaucé, Pierre Boué, Florent Brenguier, Yehuda Ben-Zion, P. E. Share, Aurélien Mordret, Chris Johnson, Thomas Lecocq, Dan Hollis, Olivier Coutant
Publikováno v:
Geophysical Research Letters
Geophysical Research Letters, American Geophysical Union, 2019, 46 (16), pp.9529-9536. ⟨10.1029/2019GL083438⟩
Geophysical Research Letters, 2019, 46 (16), pp.9529-9536. ⟨10.1029/2019GL083438⟩
Geophysical Research Letters, American Geophysical Union, 2019, 46 (16), pp.9529-9536. ⟨10.1029/2019GL083438⟩
Geophysical Research Letters, 2019, 46 (16), pp.9529-9536. ⟨10.1029/2019GL083438⟩
Laboratory experiments report that detectable seismic velocity changes should occur in the vicinity of fault zones prior to earthquakes. However, operating permanent active seismic sources to monitor natural faults at seismogenic depth is found to be
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b23e66d62cdc632fe19f0f1ad8dff052
https://hal.univ-grenoble-alpes.fr/hal-02928346
https://hal.univ-grenoble-alpes.fr/hal-02928346