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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

Published online by Cambridge University Press:  28 February 2018

Gurmeet Kaur ,
Roger H. Mitchell  and
Suhel Ahmed
Gurmeet Kaur*
Affiliation:
Department of Geology, Panjab University, Chandigarh UT-160014, India Department of Geology, Lakehead University, Thunder Bay, Ontario P7B 5E1, Canada
Roger H. Mitchell
Affiliation:
Department of Geology, Lakehead University, Thunder Bay, Ontario P7B 5E1, Canada
Suhel Ahmed
Affiliation:
Geological Survey of India, Southern Region, Hyderabad - 500 068, Andhra Pradesh, India
*
*E-mail:[email protected]
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Abstract

The mineralogy of nine recently discovered dykes (VL1:VL8 and VL10) in the vicinity of Vattikod village, Nalgonda district in Telangana State is described. The mineral assemblage present and their compositions are comparable to those of bona fide lamproites in terms of the presence of phlogopite (Ti-rich, Al-poor phlogopite and tetraferriphlogopite); amphiboles (potassic-arfvedsonite, potassic-richterite, potassic-ferro-richterite, potassic-katophorite, Ti-rich potassic-katophorite, Ti-rich potassic-magnesio-katophorite); Al-poor clinopyroxenes; feldspars (K-feldspar, Ba-K-feldspar and Na-feldspar) and spinels (chromite-magnetite and qandilite-ulvöspinel-franklinite). These dykes have undergone diverse and significant degrees of deuteric alteration as shown by the formation of secondary phases such as: titanite, allanite, hydro-zircon, calcite, chlorite, quartz and cryptocrystalline SiO2. On the basis of their respective mineralogy: the VL4 and VL5 dykes are classified as pseudoleucite-phlogopite lamproite; VL2 and VL3 dykes as pseudoleucite-amphibole-lamproite; and VL6, VL7 and VL8 as pseudoleucite-phlogopite-amphibole-lamproite. VL10 is extensively altered but contains fresh euhedral apatite microphenocrysts together with pseudomorphs after leucite and is classified as a pseudoleucite-apatite-(phlogopite?) lamproite. The mineralogy of the Vattikod lamproite dykes is compared with that of the Ramadugu, Somavarigudem and Yacharam lamproite dykes which also occur in the Ramadugu lamproite field. The lamproites from the Eastern Dharwar Craton are considered as being possible expressions of ancient subduction-related alkaline magmatism along the Eastern Ghats mobile belt.

Keywords

lamproitepseudoleucitephlogopiteK-Na-amphibolesVattikodEastern Dharwar Cratonsubduction
Type
Article
Information
Mineralogical Magazine , Volume 82 , Issue 1 , February 2018 , pp. 35 - 58
Copyright
Copyright © Mineralogical Society of Great Britain and Ireland 2018 

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Footnotes

Associate Editor: Brian O'Driscoll

References

Ahmed, S. and Kumar, A. (2012) Search for kimberlite/lamproite in Paluvayi block in Nalgonda district, Andhra Pradesh. Geological Survey of India Report, Kolkata, India.Google Scholar
Burke, K. and Khan, S. (2006) Geoinformatic approach to global nepheline syenite and carbonatite distribution: testing a Wilson cycle model. Geosphere, 2, 53–60.Google Scholar
Chalapathi Rao, N.V. and Srivastava, R.K. (2016) Kimberlites, lamproites, lamprophyres, carbonatites, other alkaline rocks and mafic dykes from the Indian Shield: Glimpses of research (2012–2016). Proceedings Indian National Science Academy, 82(3), 515–536.Google Scholar
Chalapathi Rao, N.V., Gibson, S.A., Pyle, D.M., 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
Chakrabarti, R., Basu, A.R. and Paul, D.K. (2007) Nd-Hf-Sr-Pb isotopes and trace element geochemistry of Proterozoic lamproites from southern India: subducted komatiite in the source. Chemical Geology, 236, 291–302.Google Scholar
Chalapathi Rao, N.V., Creaser, R.A., Lehmann, B. and Panwar, B.K. (2013) Re-Os isotope study of Indian kimberlites and lamproites: Implications for mantle source and cratonic evolution. Chemical Geology, 353, 36–47.CrossRefGoogle 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.CrossRefGoogle Scholar
Conticelli, S. (1998) The effect of crustal contamination on ultrapotassic magmas with lamproitic affinity: mineralogical, geochemical and isotope data from the Torre Alfina lavas and xenoliths, central Italy. Chemical Geology, 149, 51–81.CrossRefGoogle Scholar
Das Sharma, S. and Ramesh, D.S. (2013) Imaging mantle lithosphere for diamond prospecting in southeast India. Lithosphere, 5, 331–342.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.CrossRefGoogle Scholar
Dongre, A.N., Jacob, D.E. and Stern, R.A. (2015) Subduction-related origin of eclogite xenoliths from the Wajrakarur kimberlite field, Eastern Dharwar craton, Southern India: Constraints from petrology and geochemistry. Geochimica et Cosmochimica Acta, 166, 165–188.Google Scholar
Edgar, A.D. (1989) Barium- and strontium-enriched apatites in lamproites from West Kimberley, Western Australia. American Mineralogist, 74, 889–895.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
Gopalan, K. and Kumar, A. (2008) Phlogopite K–Ca dating of Narayanpet kimberlites, South India: implications to the discordance between their Rb–Sr, Ar/Ar ages. Precambrian Research, 167, 377–382.Google Scholar
Gupta, S., Rai, S.S., Prakasam, K.S., Srinagesh, D., Chadha, R.K., Priestley, K. and Gaur, V.K. (2003) First evidence for anomalous thick crust beneath mid-Archaean western Dharwar craton. Current Science, 84, 1219–1226.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, 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.). 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, Abstract #3482. Available at: https://www.americangeosciences.org/igc/15421Google Scholar
Jaques, A.L., Lewis, J.D. and Smith, C.B. (1986) The Kimberlites and Lamproites of Western Australia. Geological Survey of Western Australia Bulletin, 132.Google Scholar
Kumar, A., Ahmed, S., Priya, R. and Sridhar, M. (2013 a) 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.CrossRefGoogle Scholar
Kumar, B. Niraj, Zeyen, H., Singh, A.P. and Singh, B. (2013 b) Lithospheric structure of southern Indian shield and adjoining oceans: integrated modelling of topography, gravity, geoid and heat flow data. Geophysical Journal International, 194, 30–44.Google Scholar
Leelanandam, C., Burke, K., Ashwal, L.D. and Webb, S.J. (2006) Proterozoic mountain building in Peninsular India: an analysis based primarily on alkaline rock distribution. Geological Magazine, 143, 195–212.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. Canadian Mineralogist, 43, 795–812.CrossRefGoogle Scholar
Mirnejad, H. and Bell, K. (2006) Origin and source evolution of the Leucite Hills lamproites: evidence from Sr–Nd–Pb–O isotopic compositions. Journal of Petrology, 47, 2463–2489.Google Scholar
Mitchell, R.H. (1986) Kimberlites: Mineralogy, Geochemistry and Petrology. Plenum Press, New York and London, 442 pp.Google Scholar
Mitchell, R.H. (1989) Compositional variation of micas from the Leucite hills lamproites. 28th International Geological Congress. Washington, USA. Extended Abstract 2, pp. 446–447.Google Scholar
Mitchell, R.H. (1991) Kimberlites and Lamproites: Primary Source of Diamond. Geoscience Canada Reprint series 6, pp. 8–28.Google Scholar
Mitchell, R.H. (1995) Kimberlites, Orangeites, and Related Rocks. Plenum press. New York, 410 pp.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.CrossRefGoogle 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.CrossRefGoogle Scholar
Neelkantam, S. (2001) Exploration for diamonds in southern India. Geological Survey of India Special Publication, 58, 521–555.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.CrossRefGoogle Scholar
Osborne, I., Sherlock, S., Anand, M. and Argles, T. (2011) New Ar–Ar ages of southern Indian kimberlites and a lamproite and their geochemical evolution. Precambrian Research, 189, 91–103.Google Scholar
Perez-Valera, L.A., Rosenbaum, G., Sanchez-Gomez, M., Azor, A., Fernandez-Soler, J.M., Perez-Valera, F. and Vasconcelos, P.M. (2013) Age distribution of lamproites along the Socovos Fault (southern Spain) and lithospheric scale tearing. Lithos, 180–181, 252–263.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
Roy, S. and Mareschal, J.C. (2011) Constraints on the deep thermal structure of the Dharwar craton, India, from heat flow, shear wave velocities, and mantle xenoliths. Journal of Geophysical Research, 116, 1–15.Google Scholar
Shaikh, A.M., Patel, S.C., Ravi, S., Behera, D. and Pruseth, K.L. (2016) 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
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. Organized 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
Tappe, S., Jenner, G.A., Foley, S.F., Heaman, L., Besserer, D., Kjarsgaard, B.A. and Ryan, B. (2004) Torngat ultramafic lamprophyres and their relation to the North Atlantic Alkaline Province. Lithos, 76, 491–518.CrossRefGoogle Scholar
Tappe, S, Foley, S.F., Jenner, G.A., Heaman, L.M., Kjarsgaard, B.A., Romer, R.L., Stracke, A., Joyce, N. and Hoefs, J. (2006) Genesis of ultramafic lamprophyres and carbonatites at Aillik Bay, Labrador: a consequence of incipient lithospheric thinning beneath the North Altantic craton. Journal of Petrology, 47, 1261–1315.Google 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.CrossRefGoogle Scholar
Tappe, S., Kjarsgaard, B.A., Kurszlaukis, S., Nowell, G. and Phillips, D. (2014) Petrology and Nd-Hf isotope geochemistry of the Neoproterozoic Amon kimberlite sills, Baffin Island (Canada): Evidence for deep mantle magmatic activity linked to supercontinent cycles. Journal of Petrology, 55, 2003–2042.CrossRefGoogle Scholar
Thy, P., Stecher, O. and Korstgard, J.A. (1987) Mineral chemistry and crystallization sequences in kimberlite and lamproite dikes from the Sisimut area, central west Greenland. Lithos, 20, 391–417.CrossRefGoogle 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
Zurevinski, S.E. and Mitchell, R.H. (2011) Highly evolved hypabyssal kimberlite sills from Wemindji, Quebec, Canada: insights into the process of flow differentiation in kimberlite magmas. Contributions to Mineralogy and Petrology, 161, 765–776.Google Scholar
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