Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/44415
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dc.contributor.authorClark, C.en
dc.contributor.authorHand, M.en
dc.contributor.authorKelsey, D.en
dc.contributor.authorGoscombe, B.en
dc.date.issued2007en
dc.identifier.citationJournal of the Geological Society, 2007; 164(5):937-940en
dc.identifier.issn0016-7649en
dc.identifier.issn2041-479Xen
dc.identifier.urihttp://hdl.handle.net/2440/44415-
dc.description© 2007 Geological Society of Londonen
dc.description.abstractThe Strangways Metamorphic Complex in central Australia is a key terrane in models for the evolution of the Australian continent. The Arunta Complex preserves a long-lived (c. 1700–320 Ma) record of crustal reworking, the drivers of which are the subject of considerable debate. Pressure–temperature data and in situ monazite geochronology constrain the reworking to be coincident with the c.1645 Ma Liebig Orogeny. This suggests that reworking in the Strangways Metamorphic Complex is related to terrane accretion rather than other factors such as anomalous enrichment in high-heat-producing elements or within-plate processes.en
dc.description.statementofresponsibilityC. Clark, M. Hand, D.E. Kelsey and B. Goscombeen
dc.language.isoenen
dc.publisherGeological Soc Publ Houseen
dc.source.urihttp://jgs.geoscienceworld.org/cgi/content/abstract/164/5/937en
dc.titleLinking crustal reworking to terrane accretionen
dc.typeJournal articleen
dc.identifier.rmid0020072864en
dc.identifier.doi10.1144/0016-76492006-175en
dc.identifier.pubid47403-
pubs.library.collectionEarth and Environmental Sciences publicationsen
pubs.verification-statusVerifieden
pubs.publication-statusPublisheden
dc.identifier.orcidHand, M. [0000-0003-3743-9706]en
Appears in Collections:Earth and Environmental Sciences publications
Environment Institute publications

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