Constraining the prograde and retrograde P-T paths of granulites using decomposition of initially zoned garnets: an example from the Central Indian Tectonic Zone-Reference-Cited by-同舟云学术

Constraining the prograde and retrograde P-T paths of granulites using decomposition of initially zoned garnets: an example from the Central Indian Tectonic Zone

Published:2004-04-01 Issue:5 Volume:147 Page:581-603
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contrib Mineral Petrol

Author:

Bhowmik Santanu Kumar,Spiering Beate

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/s00410-004-0573-3.pdf

Reference52 articles.

1. Acharyya SK, Roy A (2000) Tectonothermal history of the Central Indian Tectonic Zone and reactivation of major faults/shear zones. J Geol Soc India 55:239–256

2. Berman RG, Aranovich LY (1996) Optimized standard state and solution properties of minerals. I. Model calibration for olivine, orthopyroxene, cordierite, garnet, and ilmenite in the system FeO-MgO-CaO-Al2O3-TiO2-SiO2. Contrib Mineral Petrol 126:1–24

3. Bhattacharya A, Mazumdar AC, Sen SK (1988) Fe-Mg mixing in cordierite: constraints from natural data and implications for cordierite-garnet geothermometry in granulites. Am Mineral 73:338–344

4. Bhowmik SK, Roy A (2003) Garnetiferous metabasites from the Sausar Mobile Belt:Petrology, P-T path and implications for the tectonothermal evolution of the Central Indian Tectonic Zone. J Petrol 44:387–420

5. Bhowmik SK, Pal T, Pant NC, Shome S (2000) Implication of Ramakona cordierite gneiss in the crustal evolution of Sausar mobile belt in Central India. Proceedings Volume of the International Seminar on “Precambrian Crust in Eastern and Central India. IGCP-368, Bhubaneshwar, 1998, pp 131–150

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