Abstract
Abstract The location of possible source vents for the Whakamaru Ignimbrite was investigated using flow directions inferred from anisotropy of magnetic susceptibility (AMS). If we assume that the magnetic fabric was formed in response to processes in the formative pyroclastic flow, the magnetic lineation is related to the direction to the source vent. Lineation vectors mostly appear to dip towards the source, suggesting a flow‐related imbrication of the fabric. AMS has been determined at 22 sites around Lake Taupo, and show an average bulk magnetic susceptibility (MS) of 8.04 × 10‐3 SI. The degree of anisotropy (P) ranges from 1.014 to 1.032. The magnetic susceptibility is due to titanomagnetite. Measurements showing strongly dipping magnetic foliations presumably caused by underlying topography and local deflections of the flow have been discarded. The magnetic lineation is dipping towards the source in 14 sites and 180° from the source in four sites. Four source vents for the Whakamaru Ignimbrite are in...
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