Visualizing the sedimentary response through the orogenic cycle: a multi-dimensional scaling approach

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Visualizing the sedimentary response through the orogenic cycle: a multi-dimensional scaling approach

Changing patterns in detrital provenance through time have the ability to resolve salient features of an orogenic cycle. Such changes in the age spectrum of detrital minerals may be attributable to fluctuations in the geodynamic regime (e.g., opening of seaways, initiation of subduction and arc magm...

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Bibliographic Details
Main Authors:	Spencer, Christopher, Kirkland, C.
Format:	Journal Article
Published:	2016
Online Access:	http://hdl.handle.net/20.500.11937/19652

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