Hot orogens and supercontinent amalgamation: A Gondwanan example from southern India

Author:

Clark Chris,Healy David,Johnson Tim,Collins Alan S.,Taylor Richard J.,Santosh M.,Timms Nicholas E.

Funder

Curtin University

Australian Research Council

Australia-India Strategic Research Fund

Australian Research Council Future Fellowship Scheme

ARC Centre of Excellence for Core to Crust Fluid Systems

Publisher

Elsevier BV

Subject

Geology

Reference120 articles.

1. The application of single zircon evaporation and model Nd ages to the interpretation of polymetamorphic terrains: an example from the Proterozoic mobile belt of south India;Bartlett;Contributions to Mineralogy and Petrology,1998

2. Himalayan tectonics explained by extrusion of a low-viscosity crustal channel coupled to focused surface denudation;Beaumont;Nature,2001

3. Crustal channel flows: 1. Numerical models with applications to the tectonics of the Himalayan–Tibetan orogen;Beaumont;Journal of Geophysical Research - Solid Earth,2004

4. Models of large, hot orogens containing a collage of reworked and accreted terranes;Beaumont;Canadian Journal of Earth Sciences,2010

5. Sm–Nd model ages and Rb–Sr isotope systematics of charnockites and gneisses across the Cauvery Shear Zone, southern India: implications for the Archaean-Neoproterozoic boundary in the southern granulite terrain;Bhaskar Rao,2003

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