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Mineralogy of the baotite-bearing Gundrapalli lamproite, Nalgonda district, Telangana, India

Published online by Cambridge University Press:  31 January 2019

Gurmeet Kaur  and
Roger H. Mitchell
Gurmeet Kaur*
Affiliation:
Department of Geology, Panjab University, Chandigarh UT-160014, India Department of Geology, Lakehead University, Thunder Bay Ontario, Canada P7B 5E1
Roger H. Mitchell
Affiliation:
Department of Geology, Lakehead University, Thunder Bay Ontario, Canada P7B 5E1
*
*Author for correspondence: Gurmeet Kaur, Email: [email protected]
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Abstract

We describe the mineralogy of a lamproite dyke from Gundrapalli village (Nalgonda district), Telangana, India. The dyke consists of a mineral assemblage characteristic of lamproites in terms of the presence of amphiboles (mainly potassic-richterite together with potassic-arfvedsonite, magnesio-riebeckite, Ti-rich potassic-magnesio-arfvedsonite, potassic-magnesio-arfvedsonite, katophorite and potassic-ferri-katophorite), Al-poor pyroxene, phlogopite (Ti-rich, Al-poor), pseudomorphed leucite, spinel (chromite-magnesiochromite), fluorapatite, baryte, titanite, rutile, barytocalcite, calcite, ilmenite, hydro-zircon, baotite, strontianite, allanite, quartz and pyrite. The absence of wadeite and priderite have been compensated for by the presence of baotite, rutile, titanite, baryte and hydro-zircons. The presence of the secondary phases: allanite, hydro-zircon, chlorite, quartz and cryptocrystalline silica, implies that the dyke has undergone deuteric alteration. On the basis of its typomorphic mineralogy the Gundrapalli dyke has been classified as a pseudoleucite-phlogopite-amphibole-lamproite. We report the presence of the rare mineral baotite from this lamproite, the first recognition of baotite from a lamproite in India. The mineralogy of the baotite-bearing Gundrapalli lamproite is analogous to the baotite-bearing Kvaløya lamproite from Troms, Norway.

Keywords

lamproitemineralogybaotiteGundrapalliIndiaKvaløyaNorway
Type
Article
Information
Mineralogical Magazine , Volume 83 , Issue 3 , June 2019 , pp. 401 - 411
Copyright
Copyright © Mineralogical Society of Great Britain and Ireland 2019 

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Footnotes

Associate Editor: Katharina Pfaff

References

Ahmed, S. and Kumar, A. (2012) Search for Kimberlite/lamproite in Paluvayi Block in Nalgonda District, Andhra Pradesh. Geological Survey of India Report. Kolkotta, India. www.portal.gsi.gov.in.Google Scholar
Chakhmouradian, A.C. and Mitchell, R.H. (2002) The mineralogy of Ba- and Zr-rich alkaline pegmatites from Gordon Butte, Crazy Mountains (Montana, USA): comparisons between potassic and sodic agpaitic pegmatites. Contributions to Mineralogy and Petrology, 143, 93–114.Google Scholar
Chalapathi Rao, N.V., Gibson, S.A., Pyle, D.M. and Dickin, A.P. (2004) Petrogenesis of Proterozoic lamproites and kimberlites from the Cuddapah Basin and Dharwar craton, southern India, Journal of Petrology, 45(5), 907–948.Google Scholar
Chalapathi Rao, N.V., Kamde, G., Kale, H.G. and Dongre, A. (2010) Mesoproterozoic lamproites from the Krishna Valley, Eastern Dharwar craton, southern India: petrogenesis and diamond prospectivity. Precambrian Research, 177, 103–130.Google Scholar
Chalapathi-Rao, N.V., Wu, F.Y., Mitchell, R.H., Li, Q.L. and Lehmann, B. (2013) Mesoproterozoic U-Pb ages, trace element and Sr-Nd isotopic composition of perovskite from kimberlites of the Eastern Dharwar craton, southern India: Distinct mantle sources and a widespread 1.1 Ga tectonomagmatic event. Chemical Geology, 353, 48–64.Google Scholar
Chalapathi Rao, N.V., Kumar, A., Sahoo, S., Dongre, A. N. and Talukdar, D. (2014) Petrology and petrogenesis of Mesoproterozoic lamproites from the Ramadugu field, NW margin of the Cuddapah basin, Eastern Dharwar craton, southern India. Lithos, 196–197, 150–168.Google Scholar
Chalapathi Rao, N.V., Atiullah, , Kumar, A., Sahoo, S., Nanda, P., Chahong, N., Lehmann, B. and Rao, K.V.S. (2016) Petrogenesis of Mesoproterozoic lamproite dykes from the Garledinne (Banganapalle) cluster, south-western Cuddapah Basin, southern India. Mineralogy and Petrology, 110, 247–268.Google Scholar
Cooper, A.F. (1996) Nb-rich baotite in carbonatites and fenites at Haast River, New Zealand. Mineralogical Magazine, 60, 473–482.Google Scholar
Davies, G.R., Stolz, A.J., Mahotkin, I.L., Nowell, G.M. and Pearson, D.G. (2006) Trace element and Sr–Pb–Nd–Hf isotope evidence for ancient, fluid-dominated enrichment of the source of Aladan shield lamproites. Journal of Petrology, 47, 1119–1146.Google Scholar
Fareeduddin, and Mitchell, R.H. (2012) Diamonds and their Source Rocks in India. Geological Society of India, Bangalore, India, 434 pp.Google Scholar
Fritschle, T., Prelević, D., Foley, S.F. and Jacob, D.E. (2013) Petrological characterization of the mantle source of Mediterranean lamproites: Indications from major and trace elements of phlogopite. Chemical Geology, 353, 267–279.Google Scholar
Gurmeet Kaur, and Mitchell, R.H. (2013) Mineralogy of the P2-West ‘Kimberlite’, Wajrakarur kimberlite field, Andhra Pradesh, India: kimberlite or lamproite? Mineralogical Magazine, 77, 3175–3196.Google Scholar
Gurmeet Kaur, and Mitchell, R.H. (2016) Mineralogy of the P-12 K-Ti-richterite diopside olivine lamproite from Wajrakarur, Andhra Pradesh, India: implications for subduction-related magmatism in eastern India. Mineralogy and Petrology, 110, 223–245.Google Scholar
Gurmeet Kaur, and Mitchell, R.H. (2017) Mineralogy of the baotite-bearing Gundrapalli lamproite, Nalgonda district, Telangana, India. 11th International Kimberlite Conference. Extended abstract 4499, 1–3.Google Scholar
Gurmeet Kaur, , Korakoppa, M., Fareeduddin, and Pruseth, K.L. (2013) Petrology of P-5 and P-13 “kimberlites” from Lattavaram kimberlite cluster, Wajrakarur Kimberlite Field, Andhra Pradesh, India: Reclassification as lamproites. Pp 183–194 in: Proceedings of the Xth International Kimberlite Conference (Pearson, D.G., Grutter, H.S., Harris, J.W., Kjarsgaard, B.A., O'brien, H., Chalapathi Rao, N.V. and Sparks, R.S.J., editors). Geological Society of India, Springer Publication.Google Scholar
Gurmeet Kaur, , Mitchell, R.H. and Ahmed, S. (2016) Typomorphic mineralogy of the Vattikod lamproites from Mesoproterozoic Ramadugu Lamproite Field, Nalgonda District, Telangana, India: A plausible manifestation of subduction-related alkaline magmatism in the Eastern Ghats Mobile Belt? 35 th International Geological Congress, South Africa Meeting. Abstract #3482. Available at https://www.americangeosciences.org/sites/default/files/igc/5423.pdfGoogle Scholar
Gurmeet Kaur, , Mitchell, R.H. and Ahmed, S. (2018) Mineralogy of the Vattikod lamproite dykes, Ramadugu Lamproite Field, Nalgonda District, Telangana: A possible expression of ancient subduction-related alkaline magmatism along Eastern Ghats Mobile Belt, India. Mineralogical Magazine, 82(1), 35–58.Google Scholar
Heinrich, E.W., Boyer, W.H. and Crowley, F.A. (1962) Baotite from Ravalli County, Montana. American Mineralogist, 47, 987–993.Google Scholar
Karpenko, V. and Pautov, L. (2002) Formation of baotite in alkaline rocks of a moraine of Dara-i-Pioz Glacier, Tadjikistan. Neues Jahrbuch Mineral Monatshefte, 10, 459–467.Google Scholar
Koneva, A.A., Konev, A.A. and Vladykin, N.V. (2008) Mineralogical peculiarities of the unique carbonatites of Beriah River. Pp. 77–79 in: Geochemistry of Magmatic Rocks: Alkaline Magmatism of Earth (Kogarko, L.N., editor). GEOKhI, St. Petersburg, Moscow [abstract, in Russian].Google Scholar
Krmíček, L., Cempírek, J., Havlín, A., Přichystal, A., Houzar, S., Krmíčková, M. and Gadas, P. (2011) Mineralogy and petrogenesis of a Ba–Ti–Zr-rich peralkaline dyke from Sebkovice (Czech Republic): recognition of the most lamproitic Variscan intrusion. Lithos, 121, 74–86.Google Scholar
Kullerud, K (1995) Chlorine, titanium and barium-rich biotites: factors controlling biotite composition and implications for garnet-biotite geothermometry. Contributions to Mineralogy and Petrology, 120, 42–59.Google Scholar
Kullerud, K (1996) Chlorine-rich amphiboles: interplay between amphibole composition and an evolving fluid. European Journal of Mineralogy, 8, 355–370.Google Scholar
Kullerud, K., Zozulya, D., Bergh, S.G., Hansen, H. and Ravna, E.J.K. (2011) Geochemistry and tectonic setting of a lamproite dyke in Kvaløya, North Norway. Lithos, 126, 278–289.Google Scholar
Kullerud, K., Zozulya, D. and Ravna, E. (2012) Formation of baotite – a Cl-rich silicate-together with fluorapatite and F-rich hydrous silicates in the Kvaloya lamproite dyke, North Norway. Minerlogy and Petrology, 105, 145–156.Google Scholar
Kumar, A., Heaman, L.M. and Manikyamba, C. (2007) Mesoproterozoic kimberlites in south India: A possible link to 1.1 Ga global magmatism. Precambrian Research. 154(3–4), 192–204.Google Scholar
Kumar, A., Ahmed, S., Priya, R. and Sridhar, M. (2013) Discovery of lamproites near Vattikod area, NW margin of the Cuddapah basin, Eastern Dharwar craton, southern India. Journal of the Geological Society of India, 82, 307–312.Google Scholar
Liferovich, R.P. and Mitchell, R.H. (2005) Composition and paragenesis of Na-, Nb-, and Zr-bearing titanite from Khibina, Russia, and crystal structure data for synthetic analogues. The Canadian Mineralogist, 43, 795–812.Google Scholar
Mitchell, R.H. (1989) Compositional variation of micas from the Leucite hills lamproites. 28 th International Geological Congress, Washington. Extended Abstract 2, pp.446–447.Google Scholar
Mitchell, R.H. (1995) Kimberlites, Orangeites, and Related Rocks. Plenum press. New York, 410pp.Google Scholar
Mitchell, R.H. (2006) Potassic magmas derived from metasomatized lithospheric mantle: Nomenclature and relevance to exploration for diamond-bearing rocks. Journal Geological Society of India, 67, 317–327.Google Scholar
Mitchell, R.H. and Bergman, S.C. (1991) Petrology of Lamproites. Plenum Press, New York, 447pp.Google Scholar
Mitchell, R.H. and Fareeduddin, (2009) Mineralogy of peralkaline lamproites from the Raniganj Coalfield, India. Mineralogical Magazine, 73, 457–477.Google Scholar
Mitchell, R.H. and Tappe, S. (2010) Discussions of ‘Kimberlites and aillikites as probes of the continental lithospheric mantle’. Lithos, 109, 72–80.Google Scholar
Murphy, D.T., Collerson, K.D. and Kamber, B.S. (2002) Lamproites from Gaussberg, Antarctica: Possible transition zone melts of Archaean subducted sediments. Journal of Petrology, 43, 981–1001.Google Scholar
Neelkantam, S. (2001) Exploration for diamonds in southern India. Geological Survey of India Special Publication, 58, 521–555.Google Scholar
Nemec, D. (1987) Baotite – a rock-forming mineral of Ba-rich hyperpotassic dyke rocks. Neues Jahrbuch Mineral Monatshefte, 1, 31–42.Google Scholar
Nowell, G.M., Pearson, D.G., Bell, D.R., Carlson, R.W., Smith, C.B., Kempton, P.D. and Noble, S.R. (2004) Hf isotope systematics of kimberlites and their megacrysts: New constraints on their source regions. Journal of Petrology, 45, 1583–1612.Google Scholar
Obodda, H.P. and Leavens, P.B. (2004) Zagi mountain – Northwest frontier province, Pakistan. Mineralogical Records, 35, 205–220.Google Scholar
Peng, C.J. (1959) The discovery of several new minerals of rare elements. American Mineralogist, 45, 7–45Google Scholar
Potter, E.G. and Mitchell, R.H. (2005) Mineralogy of the Deadhorse Creek volcaniclastic breccia complex, northwestern Ontario, Canada. Contributions to Mineralogy and Petrology, 150, 212–229.Google Scholar
Prelevic, D., Foley, S.F., Romer, R.L. and Conticelli, S. (2008) Mediterranean Tertiary lamproites derived from multiple source components in postcollisional geodynamics. Geochimica et Cosmochimica Acta, 72, 2125–2156.Google Scholar
Rapp, R.P., Irifune, T., Shimizu, N., Nishiyama, N., Norman, M.D. and Inoue, J. (2008) Subduction recycling of continental sediments and the origin of geochemically enriched reservoirs in the deep mantle. Earth Planetary Science Letters, 271, 14–23.Google Scholar
Rudashevsky, V.N., Gorkovetz, V.Ya., Rudashevsky, N.S., Popov, M.G. and Raevskaya, M.B. (2011) Lamproites of the Kostomuksha ore area, West Karelia (mineralogy and 3D-method of investigation). Pp. 167–168 in: Ore Potential of Alkaline, Kimberlitic and Carbonatitic Magmatism (Kogarko, L.N., editor). Pravo i economica, Moscow – Minsk [abstract, in Russian].Google Scholar
Semenov, E.I., Khun, V.S. and Kapitonova, T.A. (1961) Baotite, a new niobian mineral. Doklady AN USSR, 136, 915–916 [in Russian].Google Scholar
Shaikh, A.M., Kumar, S.P., Patel, S.C., Thakur, S.S., Ravi, S. and Behera, D. (2018) The P3 kimberlite and P4 lamproite, Wajrakarur kimberlite field, India: mineralogy, and major and minor element compositions of olivines as records of their phenocrystic vs xenocrystic origin. Mineralogy and Petrology, 11th IKC volume, 112(Suppl 2), 609, https://doi.org/10.1007/s00710-018-0562-2Google Scholar
Shaikh, A.M., Patel, S.C., Ravi, S., Behera, D. and Pruseth, K.L. (2017) Mineralogy of the TK1and TK4 ‘kimberlite’ in the Timmasamudram cluster, Wajrakarur Kimberlite Field, India: Implications for lamproite magmatism in a field of kimberlites and ultramafic lamprophyres. Chemical Geology, 455, 208–230.Google Scholar
Shuriga, T.N., Ryabeva, E.G. and Dubakina, L.S. (1980) Baotite – a new finding in the USSR. Doklady AN SSSR, 252, 1220–1223 [in Russian].Google Scholar
Sridhar, M. and Rau, T.K. (2005) Discovery of a new lamproite field Ramadugu lamproite field (RLF), Nalgonda District, Andhra Pradesh. Proceedings of the Group Discussion on Kimberlites and Related Rocks of India. Organised by the Geological Society of India, Bangalore, pp. 55–57 [Extended abstracts].Google Scholar
Tainton, K.M. and Mckenzie, D. (1994) The generation of kimberlites, lamproites and their source rocks. Journal of Petrology, 35, 787–817.Google Scholar
Talukdar, D., Pandey, A., Chalapathi Rao, N.V., Kumar, A., Belyatsky, B. and Lehmann, B. (2018) Petrology and geochemistry of the Mesoproterozoic Vattikod lamproites, Eastern Dharwar Craton, southern India: evidence for multiple enrichment of sub-continental lithospheric mantle and links with amalgamation and break-up of the Columbia supercontinent. Contributions to Mineralogy and Petrology, 173, 67, https://doi.org/10.1007/s00410-018-1493-yGoogle Scholar
Tappe, S., Foley, S.F., Stracke, A., Romer, R.L., Kjarsgaard, B.A., Heaman, L.M. and Joyce, N. (2007) Craton reactivation on the Labrador sea margins:40Ar/39Ar age and Sr-Nd-Hf-Pb isotope constraints from alkaline and carbonatites intrusive. Earth and Planetary Science Letters, 256, 433–454.Google Scholar
Tappe, S., Pearson, D.G. and Prevelic, D. (2013) Kimberlite, carbonatite, and potassic magmatism as part of the geochemical cycle. Chemical Geology, 353, 1–3.Google Scholar
Tappe, S., Smart, K., Torsvik, T., Massuyeau, M. and de Wit, M. (2018 a) Geodynamics of kimberlites on a cooling Earth: clues to plate tectonic evolution and deep volatile cycles. Earth Planet Science Letters, 484, 1–14.Google Scholar
Tappe, S., Dongre, A., Liu, C.Z. and Wu, F.Y. (2018 b) 'Premier' evidence for prolonged kimberlite pipe formation and its influence on diamond transport from deep Earth. Geology, 46, 843–846.Google Scholar
Tommasini, S., Avanzinelli, R. and Conticelli, S. (2011) The Th/La and Sm/La conundrum of the Tethyan realm lamproites. Earth and Planetary Science Letters, 301, 469–478.Google Scholar
Wagner, C. and Velde, D. (1986) The mineralogy of K-richterite-bearing lamproites. American Mineralogist, 71, 17–37.Google Scholar
Wall, F., Williams, C.T. and Woolley, A.R. (1996) Pyrochlore from weathered carbonatites at Lueshe, Zaire. Mineralogical Magazine, 60, 731–750.Google Scholar
Woolley, A.R., Bergman, S.C., Edgar, A.D., LeBas, M.J., Mitchell, R.H., Rock, N. and Scott Smith, B. (1996) Classification of lamprophyres, lamproite, kimberlite and the kalsilitic, melilitic, and leucitic rocks. The Canadian Mineralogist, 34,175–186.Google Scholar
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