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TitleThe role of phase changes in the development of forearc basins
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AuthorRogers, G C
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. 147, https://doi.org/10.4095/299064 (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; Willamette Valley; Gulf of Corcovado; Great Longitudinal Valley; Seto Inland Sea; Osaka; United States; Canada; Chile; Japan
Lat/Long WENS-126.0000 -122.0000 49.0000 47.0000
Lat/Long WENS -73.0000 -72.0000 -36.0000 -45.5000
Lat/Long WENS 130.0000 136.0000 35.0000 34.0000
Subjectstectonics; marine geology; subduction zones; plate tectonics; tectonic elements; tectonic environments; tectonic interpretations; metamorphism; subduction; lithosphere; oceanic lithosphere; mantle; Cascadia Subduction Zone; Juan de Fuca Plate
Released2016 08 31
GEOSCAN ID299064