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TitleThree-dimensional structure of the Cascadia forearc region from SHIPS active experiment and earthquake observations: tomographic inversion provides a high-resolution view into the core of the Cascadia forearc complex
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AuthorCrosson, R S; Symons, N P; Creager, K C; Preston, L A; Van Wagoner, T; Brocher, T M; Fisher, M A; SHIPS98 Working Group
SourceThe Cascadia subduction zone and related subduction systems - seismic structure, intraslab earthquakes and processes, and earthquake hazards; by Kirby, S (ed.); Wang, K (ed.); Dunlop, S (ed.); Geological Survey of Canada, Open File 4350, 2002 p. 33-34, https://doi.org/10.4095/222492 (Open Access)
LinksOnline - En ligne
Year2002
Alt SeriesUnited States Geological Survey, Open-file Report 02-328
PublisherNatural Resources Canada
MeetingIntraslab Earthquakes in the Cascadia Subduction System: Science and Hazards; Victoria; CA; September 18-21, 2000
Documentopen file
Lang.English
Mediaon-line; digital
RelatedThis publication is contained in Kirby, S; Wang, K; Dunlop, S; (2002). The Cascadia subduction zone and related subduction systems - seismic structure, intraslab earthquakes and processes, and earthquake hazards, Geological Survey of Canada, Open File 4350
File formatpdf
ProvinceWestern offshore region
NTS92A; 92B
AreaGeorgia Strait; Puget Sound; Juan de Fuca Sound; United States; Canada
Lat/Long WENS-126.0000 -122.0000 49.0000 47.0000
Subjectstectonics; structural geology; geophysics; subduction zones; plate tectonics; tectonic elements; tectonic environments; tectonic interpretations; plate motions; subduction; lithosphere; oceanic lithosphere; deformation; seismicity; seismic surveys; seismic surveys, ship; Cascadia Subduction Zone; Cascadia Margin; Juan de Fuca Plate; Juan de Fuca Slab; Mendocino Transform; SHIPS; geological hazards; intraslab earthquakes; seismic tomography surveys; tomographic inversion; Cenozoic
Released2002 06 11; 2016 08 31
GEOSCAN ID222492