Collaborative Research: Follow on to Seafloor Optical Fiber Strainmeters for the Detection of Slow Slip Events in Cascadia
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The Cascadia subduction zone lies offshore Oregon and Washington. This region is known for slow-slip events, where the plates gradually slip past each other slowly over days, weeks, or months. Onshore instrumentation can detect slow slip, but seafloor instrumentation is needed to monitor the full subduction zone. This is important because slow…
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