ABSTRACT
We conducted a land streamer survey over an existing void in southern Arizona. We apply a 2D time-domain Full-waveform inversion (FWI) method to the acquired data set. With field data examples, we demonstrate that the tunnel signature can be accurately identified in the inverted shear-wave velocity (Vs) profiles
Presentation Date: Thursday, October 18, 2018
Start Time: 8:30:00 AM
Location: 204A (Anaheim Convention Center)
Presentation Type: Oral
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2018. Society of Exploration Geophysicists
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