1887

Abstract

An array of 4.5 Hz geophone and FBAs recorded a sequence of seismicity during a hydraulic fracture stimualtion that culminated in a couple ~M3 events. These sensors record accelerations and velocities that can be used to show the peak ground motions that are necessary for seismic hazard studies. We discuss that using the appropriate instrumentation during these monitoring efforts is essential to being able to quantigy hazard.

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/content/papers/10.3997/2214-4609.20142377
2013-03-17
2024-04-18
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20142377
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