Zobrazeno 1 - 10
of 36
pro vyhledávání: '"Patricia A. McCrory"'
Autor:
Douglas S. Wilson, Patricia A. McCrory
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 23, Iss 9, Pp n/a-n/a (2022)
Abstract Widely accepted tectonic reconstructions indicate at least 100 km of coast‐parallel northwestward translation of the Sierra Nevada block of California and 15–20° clockwise rotation of most of Oregon since the current phase of Basin and
Externí odkaz:
https://doaj.org/article/92531e84901e4873925291c6ae20f056
Publikováno v:
Geology. 45:515-518
Deep, episodic slow slip on the Cascadia subduction megathrust of western North America is accompanied by low-frequency tremor in a zone of high fluid pressure between 30 and 40 km depth. Tremor density (tremor epicenters per square kilometer) varies
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1b582bcd3d4c1f1e65328841a0d3d196
https://doi.org/10.1130/g38835.1
https://doi.org/10.1130/g38835.1
Autor:
Douglas S. Wilson, Patricia A. McCrory
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1103e0edcb1d0c9591c25524ba4ed6b1
https://doi.org/10.1130/abs/2019cd-329164
https://doi.org/10.1130/abs/2019cd-329164
Publikováno v:
Geochemistry, Geophysics, Geosystems. 17:2434-2449
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a2eb4d6c280afdcb52eda338b35dced6
https://doi.org/10.1002/2015gc006198
https://doi.org/10.1002/2015gc006198
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e8588b4ffe19536ea2cda7afacfa22d5
https://doi.org/10.1130/abs/2018am-321366
https://doi.org/10.1130/abs/2018am-321366
Publikováno v:
Journal of Geophysical Research: Solid Earth. 120:4344-4358
In this study we first summarize the constraints that on the Cascadia subduction thrust, there is a 70 km gap downdip between the megathrust seismogenic zone and the Episodic Tremor and Slip (ETS) that lies further landward; there is not a continuous
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6b002caad817746e95e1a9d2f5fd3754
https://doi.org/10.1002/2015jb011920
https://doi.org/10.1002/2015jb011920
Publikováno v:
Open-File Report.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::968f5313a487a96d5664a671b39c467e
https://doi.org/10.3133/ofr20161203
https://doi.org/10.3133/ofr20161203
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fa5b102b8710affc857d29f411e7af20
https://doi.org/10.1130/abs/2017am-299789
https://doi.org/10.1130/abs/2017am-299789
Autor:
Richard G. Stanley, Anne M. Trehu, Douglas S. Wilson, G. A. Barth, Patricia A. McCrory, Daniel S. Scheirer, Robert J. McLaughlin
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::61d3d9b4a3daa8294dba76bf1e72832d
https://doi.org/10.1130/abs/2017am-299795
https://doi.org/10.1130/abs/2017am-299795
Publikováno v:
Geochemistry, Geophysics, Geosystems. 15:1071-1095
Great earthquakes anticipated on the Cascadia subduction fault can potentially rupture beyond the geodetically and thermally inferred locked zone to the depths of episodic tremor and slip (ETS) or to the even deeper fore-arc mantle corner (FMC). To e
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0d0ca06ba14bf4a395fb460a6169a824
https://doi.org/10.1002/2013gc005144
https://doi.org/10.1002/2013gc005144