Terminal tectono-magmatic phase of the New England Orogen driven by lithospheric delamination

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Terminal tectono-magmatic phase of the New England Orogen driven by lithospheric delamination

The recognition of lithospheric delamination as a mechanism for magmatism and uplift is under-recognized in the geological record. A pertinent example is the terminal phase of the New England Orogen in eastern Australia, where current explanations of slab roll-back-driven extension are incompatible...

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Bibliographic Details
Main Authors:	Olierook, Hugo, Gale, J., Pirajno, F., Jourdan, Fred, Kirkland, Chris, Evans, Noreen, McDonald, B.J., Krejci, M., Jiang, Q., Shantha Kumara, A., Mayers, C., Frew, R.A., Kaag, H., McInnes, Brent
Format:	Journal Article
Language:	English
Published:	ELSEVIER 2022
Subjects:	Science & Technology Physical Sciences Geosciences, Multidisciplinary Geology 40Ar/39Ar U-Pb Sydney Basin Bowen basin Slab roll-back EASTERN AUSTRALIA SYDNEY BASIN VOLCANIC-ROCKS TASMAN SEA CONTINENTAL LITHOSPHERE PARTITION-COEFFICIENTS GEODYNAMIC EVOLUTION INTRAPLATE VOLCANISM ISOTOPE GEOCHEMISTRY THOLEIITIC BASALTS
Online Access:	http://purl.org/au-research/grants/arc/LE130100053 http://hdl.handle.net/20.500.11937/91507

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