Seismic velocity structure associated with gas hydrate at the frontal ridge of Northern Cascadia Margin

Seismic velocity structure associated with gas hydrate at the frontal ridge of Northern Cascadia Margin

At the frontal ridge near the base of the slope off Vancouver Island, wide-angle ocean bottom seismometer (OBS) data were acquired in summer 2005, in support of the Integrated Ocean Drilling Program (IODP) Expedition 311. Marine gas hydrate is present beneath the ridge based on the observation of th...

Full description

Bibliographic Details
Main Author: Lopez, Caroll
Other Authors: Spence, George D.
Language:English
en
Published: 2010
Subjects:
Gas hydrates
Vancouver Island
Velocity
Faults
UVic Subject Index::Sciences and Engineering::Earth and Ocean Sciences
Online Access:http://hdl.handle.net/1828/2859

Internet

http://hdl.handle.net/1828/2859

Similar Items