The contorted New England Orogen (eastern Australia): New evidence from U-Pb geochronology of early Permian granitoids

A series of sharp bends (oroclines) are recognized in the Paleozoic to early Mesozoic New England Orogen of eastern Australia. The exact geometry and origin of these bends is obscured by voluminous magmatism and is still debated. Here we present zircon U‐Pb ages that confirm the lateral continuation...

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Veröffentlicht in:	Tectonics (Washington, D.C.) D.C.), 2012-02, Vol.31 (1), p.n/a
Hauptverfasser:	Rosenbaum, Gideon, Li, Pengfei, Rubatto, Daniela
Format:	Artikel
Sprache:	eng
Schlagworte:	Geological time Geology Mesozoic New England Orogen oroclinal bending oroclines Orogeny Paleozoic Permian Plate tectonics Tasmanides tectonic reconstructions Triassic U-Pb geochronology
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