Microseismicity on the Gorda Ridge
The seismicity at the northern section of the Gorda Ridge has been studied with Ocean Bottom Seismographs. Nearly one hundred earthquakes were located with RMS travel time residuals less than 0.5 seconds. Most of these events lie within or near the array and they are probably associated with the dyn...
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| Language: | en_US |
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2012
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| Online Access: | http://hdl.handle.net/1957/29324 |