Shear‐Wave Velocity Structure of Sediments on Cascadia's Continental Margin From Probabilistic Inversion of Seafloor Compliance Data

Shear‐Wave Velocity Structure of Sediments on Cascadia's Continental Margin From Probabilistic Inversion of Seafloor Compliance Data

Abstract Several seismic techniques, both passive and active, exist for estimating the shear‐wave velocity VS structure of shallow sedimentary structures. In particular, passive compliance signals recorded by broadband ocean‐bottom seismometers (OBSs) can be used to invert for VS structure. While co...

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Bibliographic Details
Main Authors: Stephen G. Mosher, Pascal Audet, Jeremy M. Gosselin
Format: Article
Language:English
Published: Wiley 2021-09-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
versus
neural networks
inverse theory
OBS
shallow sediment structure
Online Access:https://doi.org/10.1029/2021GC009720

Internet

https://doi.org/10.1029/2021GC009720

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