about
Cascadia tremor located near plate interface constrained by S minus P wave times.Metamorphic records of multiple seismic cycles during subduction.Three-dimensional variations of the slab geometry correlate with earthquake distributions at the Cascadia subduction system.Deep long-period earthquakes west of the volcanic arc in Oregon: Evidence of serpentine dehydration in the fore-arc mantle wedgeTiny intraplate earthquakes triggered by nearby episodic tremor and slip in CascadiaRegionalPwave velocity structure of the Northern Cascadia Subduction Zone
P2860
description
article publié dans la revue scientifique Science
@fr
im November 2003 veröffentlichter wissenschaftlicher Artikel
@de
scientific article published in Science
@en
wetenschappelijk artikel
@nl
наукова стаття, опублікована в листопаді 2003
@uk
name
Intraslab earthquakes: dehydration of the Cascadia slab
@en
Intraslab earthquakes: dehydration of the Cascadia slab
@nl
type
label
Intraslab earthquakes: dehydration of the Cascadia slab
@en
Intraslab earthquakes: dehydration of the Cascadia slab
@nl
prefLabel
Intraslab earthquakes: dehydration of the Cascadia slab
@en
Intraslab earthquakes: dehydration of the Cascadia slab
@nl
P2093
P356
P1433
P1476
Intraslab earthquakes: dehydration of the Cascadia slab
@en
P2093
Anne M Trehu
Kenneth C Creager
Leiph A Preston
Robert S Crosson
P304
P356
10.1126/SCIENCE.1090751
P407
P577
2003-11-14T00:00:00Z