Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/101447
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dc.contributor.authorWalsh, A.en
dc.contributor.authorHand, M.en
dc.contributor.authorKelsey, D.en
dc.date.issued2015en
dc.identifier.citationTerra Nova, 2015; 27(5):329-337en
dc.identifier.issn0954-4879en
dc.identifier.issn1365-3121en
dc.identifier.urihttp://hdl.handle.net/2440/101447-
dc.description.abstractConstraining depth–temperature conditions of syn-orogenic burial metamorphism of syn-orogenic sediments in a foreland basin provides an innovative way to investigate the thermomechanical state of the lithosphere. In central Australia, major intraplate deformation resulted in 10 km of syn-orogenic sedimentation in a basin approximately 70 km wide. The deep level of burial in the foreland of the intraplate orogen requires the involvement of weak lithosphere with an elastic thickness of ≤20 km. The profound flexural response of the foreland region indicates that major intraplate deformation in central Australia was localised into a region of dramatically weakened lithosphere.en
dc.description.statementofresponsibilityAlec K. Walsh, Martin Hand and David E. Kelseyen
dc.language.isoenen
dc.publisherWileyen
dc.rights© 2015 John Wiley & Sons Ltden
dc.titleA metamorphic perspective on foreland flexure during intraplate orogeny: evidence for the involvement of weak lithosphereen
dc.typeJournal articleen
dc.identifier.rmid0030032016en
dc.identifier.doi10.1111/ter.12164en
dc.relation.granthttp://purl.org/au-research/grants/arc/LP100200127en
dc.identifier.pubid194202-
pubs.library.collectionEarth and Environmental Sciences publicationsen
pubs.library.teamDS14en
pubs.verification-statusVerifieden
pubs.publication-statusPublisheden
dc.identifier.orcidHand, M. [0000-0003-3743-9706]en
Appears in Collections:Earth and Environmental Sciences publications

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