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See Also

These are possibly similar items as determined by title/reference text matching only.

	Pandit, M. K., Sial, A. N., Sukumaran, G. B., Pimentel, M. M., Ramasamy, A. K., & Ferreira, V. P. (2002). Depleted and enriched mantle sources for Paleo-and Neoproterozoic carbonatites of southern India: Sr, Nd, C–O isotopic and geochemical constraints. Chemical geology, 189(1-2), 69-89.
	Pandit, M.K, Sial, A.N, Sukumaran, G.B, Pimentel, M.M, Ramasamy, A.K, Ferreira, V.P (2002) Depleted and enriched mantle sources for Paleo- and Neoproterozoic carbonatites of southern India: Sr, Nd, C–O isotopic and geochemical constraints. Chemical Geology, 189 (1) 69-89 doi:10.1016/s0009-2541(02)00136-5
	Pandit, M.K., Sial, A.N., Sukumaran, G.B., Pimentel, M.M., Ramasamy, A.K., Ferreira, V.P. (2004) Reply to: Comment on “Depleted and enriched mantle sources for Paleo- and Neoproterozoic carbonatites of southern India: Sr, Nd, C-O isotopic, and geochemical constraints”. Chemical Geology, 213 (4) 435-436 doi:10.1016/j.chemgeo.2004.05.004
	Pandit, M. K., Sial, A. N., Saxena, A. D., Ferreira, V. P. (2000) Non-magmatic Features in Carbonatitic Rocks: A Re-examination of Proterozoic “Carbonatites,” Southeast Rajasthan, Northwest Indian Craton. International Geology Review, 42 (11) 1046-1053 doi:10.1080/00206810009465127
	Pandit, M. K., Sial, A. N., Ferreira, V. P. (1998) Newania Carbonatite Complex, western Indian craton: Stable isotopic evidence for mantle origin. Chinese Science Bulletin, 43. 97 doi:10.1007/bf02891535
	Kumar, A., Gopalan, K., Macdougall, J.D. (2004) Comments on: Depleted and enriched mantle sources for Paleoproterozoic and Neoproterozoic carbonatites of southern India: Sr, Nd, C–O isotopic and geochemical constraints, by M.K. Pandit et al., Chem. Geol. 189 (2002) 69–89. Chemical Geology, 213 (4) 431-433 doi:10.1016/j.chemgeo.2004.05.003
	Silva, Thyego R., Ferreira, Valderez P., Lima, Mariucha Maria C., Sial, Alcides N. (2016) Two stage mantle-derived granitic rocks and the onset of the Brasiliano orogeny: Evidence from Sr, Nd, and O isotopes. Lithos, 264. 189-200 doi:10.1016/j.lithos.2016.08.030
	Tomson, J.K., Bhaskar Rao, Y.J., Vijaya Kumar, T., Mallikharjuna Rao, J. (2006) Charnockite genesis across the Archaean–Proterozoic terrane boundary in the South Indian Granulite Terrain: Constraints from major–trace element geochemistry and Sr–Nd isotopic systematics. Gondwana Research, 10 (1) 115-127 doi:10.1016/j.gr.2005.11.023
	Roy, A., Sarkar, A., Jeyakumar, S., Aggrawal, S. K., Ebihara, M., Satoh, H. (2004) Late Archaean mantle metasomatism below eastern Indian craton: Evidence from trace elements, REE geochemistry and Sr—Nd—O isotope systematics of ultramafic dykes. Journal of Earth System Science, 113 (4). 649-665 doi:10.1007/bf02704027
	Sial, Alcides N., Campos, Marcel S., Gaucher, Claudio, Frei, Robert, Ferreira, Valderez P., Nascimento, Rielva C., Pimentel, Marcio M., Pereira, Natan S., Rodler, Alexandra (2015) Algoma-type Neoproterozoic BIFs and related marbles in the Seridó Belt (NE Brazil): REE, C, O, Cr and Sr isotope evidence. Journal of South American Earth Sciences, 61. 33-52 doi:10.1016/j.jsames.2015.04.001
	Han, B. F., Wang, S. G., Jahn, B. M., Hong, D. W., Kagami, H., & Sun, Y. L. (1997). Depleted-mantle source for the Ulungur River A-type granites from North Xinjiang, China: geochemistry and Nd–Sr isotopic evidence, and implications for Phanerozoic crustal growth. Chemical Geology, 138(3-4), 135-159.