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Title of Journal: Bull Volcanol

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Abbravation: Bulletin of Volcanology

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Springer-Verlag

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10.1007/bf01632642

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1432-0819

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Sheathfolds in rheomorphic ignimbrites

Authors: M J Branney T L Barry M Godchaux
Publish Date: 2004/02/18
Volume: 66, Issue: 6, Pages: 485-491
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Abstract

Structural reappraisal of several classic rheomorphic ignimbrites in Colorado Idaho the Canary Islands and Italy has for the first time revealed abundant oblique folds curvilinear folds and sheathfolds which formed during emplacement Like their equivalents in tectonic shearzones the sheathfold axes lie subparallel to a pervasive elongation lineation and appear as eye structures on rock surfaces normal to the transport direction With the recognition of sheathfolds ignimbrites previously inferred to have undergone complex rheomorphic deformation histories are reinterpreted as recording a single progressive deformation event In some examples the trends of sheathfolds and related lineations change with height through a single ignimbrite suggesting that rheomorphism did not affect the entire thickness of ignimbrite synchronously Instead we infer that in these ignimbrites a thin ductile shearzone rose gradually through the aggrading agglutinating mass whilst the flow direction varied with time This suggests that in some cases both welding and rheomorphism can be extremely rapid with ductile strain rates significantly exceeding rates of ignimbrite aggradation


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