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Geochemical and Geochronological Data from Charnockites and Anorthosites from India's Kodaikanal-Palani Massif, Southern Granulite Terrain, India
Date
2009-10-30
Author
Sayıt, Kaan
Catlos, Elizabeth J.
Sivasubramanian, P.
Dubey, C.S.
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https://hdl.handle.net/11511/102241
Conference Name
Portland GSA Annual Meeting
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Department of Geological Engineering, Conference / Seminar
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Geochemical and geochronological data from charnockites and anorthosites from India's Kodaikanal-Palani Massif, Southern Granulite Terrain, India
Sayıt, Kaan; Sivasubramanian, P; Dubey, C. S. (Springer, 2011-01-01)
The Kodaikanal–Palani Massif is an important component of India’sSouthern Granulite Terrain; understanding the tectonic history of its rocks lendsconsiderable insight into its role within South India. The massif is located southof the Palghat Cauvery Shear Zone (PCSZ). Compilations of available geochronologicand geochemical information from charnockites north and south of the PCSZshow these rocks largely differ in age, with northern samples recording Archaeancrystallization events, whereas those to the sout...
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K. Sayıt, E. J. Catlos, P. Sivasubramanian, and C. S. Dubey, “Geochemical and Geochronological Data from Charnockites and Anorthosites from India’s Kodaikanal-Palani Massif, Southern Granulite Terrain, India,” presented at the Portland GSA Annual Meeting, Oregon, Amerika Birleşik Devletleri, 2009, Accessed: 00, 2023. [Online]. Available: https://hdl.handle.net/11511/102241.