The P-T-t architecture of a Gondwanan suture: REE, U–Pb and Ti-in-zircon thermometric constraints from the Palghat Cauvery shear system, South India

Author:

Clark Chris,Collins Alan S.,Santosh M.,Taylor Richard,Wade Benjamin P.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference90 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. Behavior of accessory phases and redistribution of Zr, REE, Y, Th, and U during metamorphism and partial melting of metapelites in the lower crust: an example from the Kinzigite formation of Ivrea-Verbano, NW Italy;Bea;Geochimica et Cosmochimica Acta,1999

3. Sm–Nd and Rb–Sr ages and P-T history of the Archean Sittampundi and Bhavani layered meta-anorthosite complexes in Cauvery shear zone, South India: evidence for Neoproterozoic reworking of Archean crust;Bhaskar Rao;Contributions to Mineralogy and Petrology,1996

4. Sm–Nd model ages and Rb–Sr isotopic systematics of Charnockites and Gneisses across the Cauvery shear zone, Southern India: implications for the Archaean–Neoproterozoic Terrane Boundary in the Southern Granulite Terrain;Bhaskar Rao;Memoir Geological Society of India,2003

5. Terminal suturing of Gondwana and the onset of the Ross-Delamerian Orogeny: the cause and effect of an Early Cambrian reconfiguration of plate motions;Boger;Earth and Planetary Science Letters,2004

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