Climate change triggered sedimentation and progressive tectonic uplift in a coupled piedmont–axial system: Cuyama Valley, California, USA

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dc.contributor.authorDeLong, S.B.
dc.contributor.authorPelletier, J.D.
dc.contributor.authorArnold, L.J.
dc.date.issued2008
dc.description.abstractAbstract not available
dc.description.statementofresponsibilityStephen B. DeLong, Jon D. Pelletier, and Lee J. Arnold
dc.identifier.citationEarth Surface Processes and Landforms, 2008; 33(7):1033-1046
dc.identifier.doi10.1002/esp.1600
dc.identifier.issn0197-9337
dc.identifier.issn1096-9837
dc.identifier.orcidArnold, L.J. [0000-0001-9603-3824]
dc.identifier.urihttp://hdl.handle.net/2440/89825
dc.language.isoen
dc.publisherJohn Wiley & Sons
dc.rights©2007 John Wiley & Sons, Ltd.
dc.source.urihttps://doi.org/10.1002/esp.1600
dc.subjectPiedmont; Quaternary climate; sedimentation; tectonics; Cuyama Valley
dc.titleClimate change triggered sedimentation and progressive tectonic uplift in a coupled piedmont–axial system: Cuyama Valley, California, USA
dc.typeJournal article
pubs.publication-statusPublished

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