Deep crustal seismic reflection images from the Dharwar craton, Southern India—evidence for the Neoarchean subduction
Author:
Affiliation:
1. CSIR-National Geophysical Research Institute, Hyderabad 500007, India. E-mail: vijayraov@yahoo.co.in
2. Institute for Geophysics, Applied Seismology, University of Texas at Austin, Austin, TX 78712-1692, USA
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/gji/article-pdf/212/2/777/27703339/ggx427.pdf
Reference90 articles.
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2. U-Pb ages for Zircon and Titanite from the Ramagiri area, Southern India: evidence for accretionary origin of the Eastern Dharwar craton during the late Archean;Balakrishnan;J. Geol.,1999
3. A geodynamic framework for interpreting crustal-scale seismic reflectivity patterns in compressional orogens;Beaumont;Geophys. J. Int.,1994
4. Rb–Sr ages of late Archean metavolcanics and granites, Dharwar craton, South India and evidence for Early Proterozoic thermotectonic event;Bhaskar Rao;Precambrian Res.,1992
5. The emerging pattern of crust-formation and recycling history in the Precambrian Dharwar Craton and the Southern Granulite Terrain, southern India, Constraints from recent geochronological and isotopic results;Bhaskar Rao;J. Geol. Soc. India,2008
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