Please use this identifier to cite or link to this item: https://hdl.handle.net/2440/112742
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dc.contributor.authorBestland, E.-
dc.contributor.authorLiccioli, C.-
dc.contributor.authorSoloninka, L.-
dc.contributor.authorChittleborough, D.-
dc.contributor.authorFink, D.-
dc.date.issued2016-
dc.identifier.citationGeomorphology, 2016; 270:40-54-
dc.identifier.issn0169-555X-
dc.identifier.issn1872-695X-
dc.identifier.urihttp://hdl.handle.net/2440/112742-
dc.description.abstractAbstract not available-
dc.description.statementofresponsibilityErick A. Bestland, CaterinaLiccioli, Lesja Soloninka, David J.Chittleborough, David Fink-
dc.language.isoen-
dc.publisherElsevier-
dc.rights© 2016 Published by Elsevier B.V.-
dc.source.urihttp://dx.doi.org/10.1016/j.geomorph.2016.07.014-
dc.subjectCosmogenic nuclide; denudation rates; chemical weathering and erosion; Mt. Lofty Ranges; Australian geomorphology-
dc.titleCatchment-scale denudation and chemical erosion rates determined from ¹⁰Be and mass balance geochemistry (Mt. Lofty Ranges of South Australia)-
dc.title.alternativeCatchment-scale denudation and chemical erosion rates determined from (10)Be and mass balance geochemistry (Mt. Lofty Ranges of South Australia)-
dc.typeJournal article-
dc.identifier.doi10.1016/j.geomorph.2016.07.014-
pubs.publication-statusPublished-
Appears in Collections:Aurora harvest 8
Geology & Geophysics publications

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