|
[1]
|
Young, D.N., Zhao, J.X., Ellis, D.J. and McCulloch, M.T. (1997) Geochemical and Sr–Nd isotopic mapping of source provinces for the Mawson charnockites, east Antarctica: Implications for Proterozoic tectonics and Gond- wana reconstruction. Precambrian Research, 86, 1-19.
|
|
[2]
|
Subba Rao, M.V. and Divakara Rao, V. (1988) Chemical constraints on the origin of the charnockites in the Eastern Ghat Mobile Belt, India. Chemical Geology, 69, 37- 48.
|
|
[3]
|
Zhao J., Ellis D.J., Kilpatrick, J.A. and McCulloch, M.T. (1997) Geochemical and Sr-Nd isotopic study of charnockites and related rocks in the northern Prince Charles Mountain, East Antarctica. Precambrian Research, 81, 37-66.
|
|
[4]
|
Sheraton, J.W, Tindle, A.G. and Tingey, R.J. (1996) Geochemistry, origin, and tectonic setting of granitic rocks of the Prince Charles Mountains, Antarctica. Australian Journal of Geology & Geophysics, 16, 345-370.
|
|
[5]
|
Kar, R., Bhattacharya, S. and Sheraton, J.W. (2003) Horn- blende dehydration melting in mafic rocks and the link between massif-type charnockite and associated granulites, Eastern Ghats Granulite Belt, India. Contributions to Mineralalogy and Petrology, 145, 707-729.
|
|
[6]
|
Kar, R. (2010) Melting experiments in the NCFMASH system at 8 kbar: Implications for the origin of mafic granulites. Indian Journal of Geology, Special Issue on Geodynamic Regimes, Global tectonics and evolution of Precambrian cratonic basins in India. 80, 71-80.
|
|
[7]
|
Jenner, G.A., Longerich, H.P., Jackson, S.E. and Fryer, B. J. (1990) ICP-MS a powerfull tool for high-precision trace element analysis in earth science: Evidence from analysis of selected USGS reference samples, Chemical Geology, 83, 133-148.
|
|
[8]
|
Govindaraju, K. (1994) 1994 compilation of working values and sample description for 383 geostandards. Geo- standards Newsletter, 18, 1-158.
|
|
[9]
|
Tarney, J., Wyborn, L.E.A., Sheraton, J.W. and Wyborn, D. (1987) Trace element differences between Archaean, proterozoic and phanerozoic crustal components: Implications for crustal growth processes. In: Ashwal, L.D. Ed., Workshop on the growth of continental crust, Lunar and Planetary Institute, 139-140.
|
|
[10]
|
Nutman, A.P., McGregor, V.R., Friend, C.R.L., Bennet, V. C. and Kinny, P.D. (1996) Itsaq gneiss complex of southern west Greenland; the world’s most extensive record of early crustal evolution (3,900-3,600 Ma). Precambrian Research, 78, 1-39.
|
|
[11]
|
Santosh, M., Maruyama, S. and Sato, K. (2009) Anatomy of a Cambrian suture in Gondwana: Pacific-type orogeny in southern India? Gondwana Research, 16, 321-341.
|
|
[12]
|
Lal, R.K., Ackermand, D. and Upadhyay, H. (1987) P- T-X relationships deduced from corona textures in sapphirine-spinel-quartz assemblages from Paderu, southern India. Journal of Petrology, 28, 1139-1168.
|
|
[13]
|
Dasgupta, S., Sengupta, P., Fukuoka, M. and Bhattacharya, P.K. (1991) Mafic granulites in the Eastern Ghats, India: Further evidence for extremely high temperature crustal metamorphism. Journal of Geology, 99, 124-133.
|
|
[14]
|
Bhowmik, S.K., Dasgupta, S., Hoernes, S. and Bhattacharya, P.K. (1995) Extremely high-temperature calcare- ous granulites from the Eastern Ghats, India: Evidence for isobaric cooling, fluid buffering, and terminal channelized fluid flow. Europian Journal of Mineralogy, 7, 689-703.
|
|
[15]
|
Sen, S.K., Bhattacharya, S. and Acharyya, A. (1995) A multi-stage pressure-temperature record in the Chilka La- ke granulites: The epitome of the metamorphic evolution of Eastern Ghats, India? Journal of Metamorphic Geology, 13, 287-298.
|
|
[16]
|
Bhattacharya, S. and Kar, R. (2002) High-temperature dehydration melting and decompressive P T path in a granulite complex from the Eastern Ghats, India. Contributions to Mineralogy and Petrology, 143,175-191.
|
|
[17]
|
Patino Douce, A.E. and Beard, J.S. (1995) Dehydration melting of biotite gneiss and quartz amphibolite from 3 to 15 kbar. Journal of Petrology, 36, 707-738.
|
|
[18]
|
Springer, W. and Seck, H.A. (1997) Partial fusion of ba- sic granulites at 5 to 15 kbar: Implications for the origin of TTG magmas. Contributions to Mineralogy and Petrology, 127, 30-45.
|
|
[19]
|
Lopez, S. and Castro, A. (2001) Determination of the fliud-absent solidus and supersolidus phase relationships of MORB-derived amphibolites in the range 4-14 kbar. American Mineralogist, 86, 1396-1403.
|
|
[20]
|
Sisson, T.W., Ratajeski, K. and Hankins, W.B. (2005) Vo- luminous granitic magmas from common basaltic sources. Contributions to Mineralogy and Petrology, 148, 635- 661.
|
|
[21]
|
Rickers, K., Mezger, K. and Raith, M., (2001) Evolution of the continental crust in the Proterozoic Eastern Ghats Belt, India and new constraints for Rodinia reconstruction: Implications from Sm-Nd, Rb-Sr and Pb-Pb isotopes. Precambrian Research, 112, 183-210.
|
|
[22]
|
Bhui, U.K., Sengupta, P. and Sengupta, P. (2007) Phase relations in mafic dykes and their host rocks from Kondapalle, Andhra Pradesh, India: Implications for the time- depth trajectory of the Paleoproterozoic (late Archean?) granulites from southern Eastern Ghats Belt. Precambrian Research, 156, 153-174.
|
|
[23]
|
Taylor, S.R. and McLennan, S.M. (1985) The continental crust: Its composition and evolution. Blackwell, Oxford.
|