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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Hlavní autoři:	Stephen G. Mosher, Pascal Audet, Jeremy M. Gosselin
Médium:	Artigo
Jazyk:	Inglês
Vydáno:	Wiley 2021-09-01
Edice:	Geochemistry, Geophysics, Geosystems
Témata:	versus neural networks inverse theory OBS shallow sediment structure
On-line přístup:	https://doi.org/10.1029/2021GC009720
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