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

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

Internet

http://purl.org/au-research/grants/arc/LE130100053
http://hdl.handle.net/20.500.11937/91507

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