Holocene faulting in the Bellingham forearc basin: Upper‐plate deformation at the northern end of the Cascadia subduction zone

Publisher： John Wiley & Sons Inc

E-ISSN： 2156-2202|117|B3|2011JB008816-2011JB008816

ISSN： 0148-0227

Source： Journal Of Geophysical Research, Vol.117, Iss.B3, 2012-03, pp. : n/a-n/a

Disclaimer: Any content in publications that violate the sovereignty, the constitution or regulations of the PRC is not accepted or approved by CNPIEC.

Previous Menu Next

Abstract

Related content

Deformation across the forearc of the Cascadia subduction zone at Cape Blanco, Oregon

By  

Journal Of Geophysical Research, Vol. 105, Iss. B2, 2000-02 ,pp. : 3095-3102

John Wiley & Sons Inc

Access to resources Recommend Favorite

Current deformation and the width of the seismogenic zone of the northern Cascadia subduction thrust

By  

Journal Of Geophysical Research, Vol. 99, Iss. B1, 1994-01 ,pp. : 653-668

John Wiley & Sons Inc

Access to resources Recommend Favorite

A revised dislocation model of interseismic deformation of the Cascadia subduction zone

By  

Journal Of Geophysical Research, Vol. 108, Iss. B1, 2003-01 ,pp. : n/a-n/a

John Wiley & Sons Inc

Access to resources Recommend Favorite

Regional P wave velocity structure of the Northern Cascadia Subduction Zone

By  

Journal Of Geophysical Research, Vol. 111, Iss. B12, 2006-12 ,pp. : n/a-n/a

John Wiley & Sons Inc

Access to resources Recommend Favorite

Late Quaternary stream incision and uplift in the forearc of the Cascadia subduction zone, western Oregon

By  

Journal Of Geophysical Research, Vol. 100, Iss. B10, 1995-10 ,pp. : 20193-20210

John Wiley & Sons Inc

Access to resources Recommend Favorite