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Pseudotachylyte-generating faults in Central Otago, New Zealand

Barker, Shaun


In Central Otago, New Zealand, a series of subparallel, NNE-SSW trending, gently dipping (10-30° E) brittle faults are hosted in quartzofeldspathic schist. These faults contain numerous (n>100) pseudotachylyte veins. Pseudotachylyte fault veins are trace

CollectionsANU Research Publications
Date published: 2005
Type: Journal article
Source: Tectonophysics
DOI: 10.1016/j.tecto.2004.12.005


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