Middle-Late Devonian nascent back arc formation, southern New England Orogen, NSW, Australia

The New England Orogen (NEO), the youngest of the orogens of the Tasmanides of eastern Australia, is defined by two main cycles of compression-extension. The compression component involves thrust tectonics and advance of the arc towards the continental plate, while extension is characterised by rifting, basin formation, thermal relaxation and retreat of the arc towards the oceanic plate. A compilation of 623 records of presence of extensional-type magmatism in eastern Qld that occurred between 270 and 260Ma.

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Devonian–Carboniferous regional deformation in the northeastern Lachlan Orogen, southeastern Australia

Fergusson

Colquhoun

2021

Australian Journal of Earth Sciences

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Middle-Late Devonian nascent back arc formation, southern New England Orogen, NSW, Australia

Cited by 5 publications

References 63 publications

Ca. 1.04 Ga hot Grenville granites in the western Yangtze Block, southwest China

Ca. 1.04 Ga hot Grenville granites in the western Yangtze Block, southwest China

Tectonic cycles of the New England Orogen, eastern Australia: A Review

Devonian–Carboniferous regional deformation in the northeastern Lachlan Orogen, southeastern Australia

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Middle-Late Devonian nascent back arc formation, southern New England Orogen, NSW, Australia

Cited by 5 publications

References 63 publications

Ca. 1.04 Ga hot Grenville granites in the western Yangtze Block, southwest China

Ca. 1.04 Ga hot Grenville granites in the western Yangtze Block, southwest China

Tectonic cycles of the New England Orogen, eastern Australia: A Review

Devonian–Carboniferous regional deformation in the northeastern Lachlan Orogen, southeastern Australia

Contact Info

Product

Resources

About

Ca. 1.04 Ga hot Grenville granites in the western Yangtze Block, southwest China

Ca. 1.04 Ga hot Grenville granites in the western Yangtze Block, southwest China