Nature of the low velocity zone in Cascadia from receiver function waveform inversion

Earth and Planetary Science Letters

Volumn 337-338, Issue , 2012, Pages 25-38

  Hansen, Ralf T J ^a   Bostock, Michael G ^a   Christensen, Nikolas I ^a  

^a UNIVERSITY OF BRITISH COLUMBIA   (Canada)

Author keywords

Cascadia; Hydrated oceanic crust; Low velocity zone; Pore fluid pressure; Segmentation; Subduction zone

Indexed keywords

CASCADIA; LOW VELOCITY ZONES; OCEANIC CRUST; PORE FLUID PRESSURE; SUBDUCTION ZONES;

CORE DRILLING; DEHYDRATION; HYDRATION; IMAGE SEGMENTATION; STRUCTURAL GEOLOGY; TECTONICS;

WAVEFORM ANALYSIS;

BASALT; DATA INVERSION; FLUID PRESSURE; OCEANIC CRUST; PLATE BOUNDARY; PORE PRESSURE; POROSITY; SEISMIC VELOCITY; SEISMIC ZONE; SEISMOLOGY; WAVEFORM ANALYSIS;

BRITISH COLUMBIA; CALIFORNIA; CANADA; CASCADIA SUBDUCTION ZONE; PACIFIC OCEAN; UNITED STATES; VANCOUVER ISLAND;

EID: 84862330810     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2012.05.031     Document Type: Article

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