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Bhadra, Subhadip, Das, Suman, Bhattacharya, A. (2007) Shear Zone-hosted Migmatites (Eastern India): the Role of Dynamic Melting in the Generation of REE-depleted Felsic Melts, and Implications for Disequilibrium Melting. Journal of Petrology, 48 (3) 435-457 doi:10.1093/petrology/egl066

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Reference TypeJournal (article/letter/editorial)
TitleShear Zone-hosted Migmatites (Eastern India): the Role of Dynamic Melting in the Generation of REE-depleted Felsic Melts, and Implications for Disequilibrium Melting
JournalJournal of Petrology
AuthorsBhadra, SubhadipAuthor
Das, SumanAuthor
Bhattacharya, A.Author
Year2007 (March)Volume48
Issue3
PublisherOxford University Press (OUP)
DOIdoi:10.1093/petrology/egl066Search in ResearchGate
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Mindat Ref. ID177788Long-form Identifiermindat:1:5:177788:2
GUID0
Full ReferenceBhadra, Subhadip, Das, Suman, Bhattacharya, A. (2007) Shear Zone-hosted Migmatites (Eastern India): the Role of Dynamic Melting in the Generation of REE-depleted Felsic Melts, and Implications for Disequilibrium Melting. Journal of Petrology, 48 (3) 435-457 doi:10.1093/petrology/egl066
Plain TextBhadra, Subhadip, Das, Suman, Bhattacharya, A. (2007) Shear Zone-hosted Migmatites (Eastern India): the Role of Dynamic Melting in the Generation of REE-depleted Felsic Melts, and Implications for Disequilibrium Melting. Journal of Petrology, 48 (3) 435-457 doi:10.1093/petrology/egl066
In(2007, March) Journal of Petrology Vol. 48 (3) Oxford University Press (OUP)

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NABELEK, PETER. I., GLASCOCK, MICHAEL. D. (1995) REE-Depleted Leucogranites, Black Hills, South Dakota: a Consequence of Disequilibrium Melting of Monazite-Bearing Schists. Journal of Petrology, 36 (4) 1055-1071 doi:10.1093/petrology/36.4.1055
Castro, A. (2001) Plagioclase morphologies in assimilation experiments. Implications for disequilibrium melting in the generation of granodiorite rocks. Mineralogy and Petrology, 71 (1) 31-49 doi:10.1007/s007100170044
WASYLENKI, L. E. (2003) Near-solidus Melting of the Shallow Upper Mantle: Partial Melting Experiments on Depleted Peridotite. Journal of Petrology, 44 (7) 1163-1191 doi:10.1093/petrology/44.7.1163
Maheo, G., Blichert-Toft, J., Pin, C., Guillot, S., Pecher, A. (2009) Partial Melting of Mantle and Crustal Sources beneath South Karakorum, Pakistan: Implications for the Miocene Geodynamic Evolution of the India-Asia Convergence Zone. Journal of Petrology, 50 (3) 427-449 doi:10.1093/petrology/egp006
SKJERLIE, K. P. (2002) The Fluid-absent Partial Melting of a Zoisite-bearing Quartz Eclogite from 1middle dot0 to 3middle dot2 GPa; Implications for Melting in Thickened Continental Crust and for Subduction-zone Processes. Journal of Petrology, 43 (2) 291-314 doi:10.1093/petrology/43.2.291
Neogi, S., Dasgupta, S., Fukuoka, M. (1998) High P-T Polymetamorphism, Dehydration Melting, and Generation of Migmatites and Granites in the Higher Himalayan Crystalline Complex, Sikkim, India. Journal of Petrology, 39 (1) 61-99 doi:10.1093/petroj/39.1.61
Jung, S, Hoernes, S, Mezger, K (2000) Geochronology and petrology of migmatites from the Proterozoic Damara Belt — importance of episodic fluid-present disequilibrium melting and consequences for granite petrology. Lithos, 51 (3) 153-179 doi:10.1016/s0024-4937(99)00062-6
GARCIA-CASCO, A. (2003) Synthesis of Staurolite in Melting Experiments of a Natural Metapelite: Consequences for the Phase Relations in Low-Temperature Pelitic Migmatites. Journal of Petrology, 44 (10) 1727-1757 doi:10.1093/petrology/egg056
Das, Suman, Bhattacharya, Abhijit, Raith, Michael M., Bhadra, Subhadip, Banerjee, Manua (2006) Aluminous sapphirine granulites from the Eastern Ghats Belt (India): Phase relations and relevance to counterclockwise P-T history. European Journal of Mineralogy, 18 (1) 35-48 doi:10.1127/0935-1221/2006/0018-0035
BEA, F. (1996) Residence of REE, Y, Th and U in Granites and Crustal Protoliths; Implications for the Chemistry of Crustal Melts. Journal of Petrology, 37 (3) 521-552 doi:10.1093/petrology/37.3.521
Font, L., Murton, B. J., Roberts, S., Tindle, A. G. (2007) Variations in Melt Productivity and Melting Conditions along SWIR (70°E–49°E): Evidence from Olivine-hosted and Plagioclase-hosted Melt Inclusions. Journal of Petrology, 48 (8) 1471-1494 doi:10.1093/petrology/egm026
 
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