Abstract
In the March-April 2017 issue of Geophysics, we see an improved structure-tensor-based coherence technique to detect and map seismic faults and channels. We learn about a new viscoelastic reverse time migration algorithm with attenuation compensation. We also learn about a new sparse dictionary method for full-waveform inversion (FWI). In rock physics, we see a new approach to amplitude variation with offset and azimuth (AVOA) analysis that helps determine fracture fluid properties, as well as a new study of acoustic measurements in well-mated fracture environments.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
