Elastic Properties and Seismic Anisotropy Across the Alpine Fault, New Zealand

Abstract Seismically detected low‐velocity zones are commonly associated with major crustal faults. In order to accurately interpret these low‐velocity zones and understand processes that produce them, direct measurements of seismic wave speed through fault zone rocks are needed. The Alpine Fault do...

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Bibliographic Details
Main Authors: T. N. Jeppson, H. J. Tobin
Format: Article
Language:English
Published: Wiley 2020-08-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
Online Access:https://doi.org/10.1029/2020GC009073