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Mineralogy of the Marepalli lamproite dyke from the Nalgonda district, Telangana, Southern India

Published online by Cambridge University Press:  22 June 2022

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

The Marepalli dyke of the Vattikod cluster of the Ramadugu Lamproite Field, Nalgonda district, Telangana, India consists of pseudomorphed leucite, phlogopite (Al-poor, Ti-rich zoned phlogopite micas), pseudomorphed olivine, fluorapatite and Al-poor diopside embedded in groundmass consisting mainly of poikilitic Fe-rich titanian phlogopite and potassic amphibole. Other groundmass minerals are Al-Na-poor diopside, Al-poor spinels (titanian magnesian chromites to titanian chromites), Sr-rich fluorapatite and late-stage interstitial anhedral crystals of titanite and K-feldspar. The late-stage deuteric minerals present are REE-rich allanite, pyrite, magnetite, chalcopyrite, galena, hydro-zircon, carbonates (calcite, witherite and strontianite), baryte and cryptocrystalline SiO2. Apatite is an early crystallising phase and is present as inclusions in phlogopite and pyroxene. Phlogopite and amphibole occur as inclusions in titanite and K-feldspar. The compositional trends of phlogopite are of almost constant Al2O3 content with FeOT and TiO2 enrichment, and are typical of lamproitic micas. The FeOT enrichment is accompanied additionally by MgO depletion (reflecting VIFe2+ enrichment) from core to rim together with a slight increase in the tetraferric iron component. Diopside is characterised by <0.4 wt.% alumina and <0.6 wt.% sodium contents and exhibits typical lamproitic affinity. The spinels are alumina-poor with un-evolved titanian magnesian chromite to titanian chromite compositions. The presence of K-richterite, as an abundant amphibole, indicates a lamproite affinity, and on the basis of the typomorphic mineralogy, this rock is classified as a ‘pseudoleucite-amphibole-phlogopite lamproite’. The Marepalli lamproite shows significant difference in compositional ranges of phlogopite, amphibole, pyroxene and spinel in comparison to those reported from the Vattikod, Gundrapalli, Ramadugu, Somavarigudem and Yacharam lamproites of Ramadugu Lamproite Field. These lamproites are considered to form from a common parent magma under reducing conditions as evidenced from: (1) low tetraferric iron content in phlogopite; (2) low Fe3+# and Ti# in spinels; and (3) high F content in phlogopite and apatite.

Keywords

lamproitemineralogyphlogopitespinelMarepalliVattikodEastern Dharwar Craton
Type
Article
Information
Mineralogical Magazine , Volume 86 , Issue 5 , October 2022 , pp. 799 - 813
Copyright
Copyright © The Author(s), 2022. Published by Cambridge University Press on behalf of The Mineralogical Society of Great Britain and Ireland

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Footnotes

Associate Editor: Leone Melluso

References

Ahmed, S., Sufija, M.V. and Ravi, S. (2016) Final report on search for kimberlite/lamproite in Kollapur–Srirangapur blocks in parts of Mahabubnagar district, Telangana and Kurnool district, Andhra Pradesh (G-4 stage). Unpublished progress report of the Geological Survey of India for field seasons 2014–15 and 2015–16.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., Kamde, G., Kale, H.S. and Dongre, A. (2010) Petrogenesis of the Mesoproterozoic lamproites from the Krishna valley, eastern Dharwar craton, southern India. Precambrian Research 177, 103–130.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, 150–168.CrossRefGoogle Scholar
Chalapathi Rao, N.V., Giri, R.K., Sharma, A. and Pandey, A. (2020) Lamprophyres from the Indian shield: A review of their occurrence, petrology, tectonomagmatic significance and relationship with the Kimberlites and related rocks. Episodes Journal of International Geoscience, 43, 231–248.Google Scholar
Dongre, A. and Tappe, S. (2019) Kimberlite and carbonatite dykes within the Premier diatreme root (Cullinan Diamond Mine, South Africa): New insights to mineralogical-genetic classifications and magma CO2 degassing. Lithos, 338, 155–173.CrossRefGoogle Scholar
Fanlo, I., Gervilla, F., Colás, V. and Subías, I. (2015) Zn-, Mn-and Co-rich chromian spinels from the Bou-Azzer mining district (Morocco): constraints on their relationship with the mineralizing process. Ore Geology Reviews, 71, 82–98.CrossRefGoogle Scholar
Fareeduddin, and Mitchell, R.H. (2012) Diamonds and their Source Rocks in India. Geological Society of India, Bangalore, India, 434pp.Google Scholar
Foley, S.F., Taylor, W.R. and Green, D.H. (1986) The role of fluorine and oxygen fugacity in the genesis of the ultrapotassic rocks. Contributions to Mineralogy and Petrology, 94, 382–392.CrossRefGoogle Scholar
Gurmeet, Kaur and Mitchell, R.H. (2013) Mineralogy of 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. (2019) Mineralogy of the baotite-bearing Gundrapalli lamproite, Nalgonda district, Telangana, India. Mineralogical Magazine, 83, 401–411.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. (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, 35–58.Google Scholar
Jayananda, M., Santosh, M. and Aadhiseshan, K.R. (2018) Formation of Archean (3600–2500 Ma) continental crust in the Dharwar Craton, southern India. Earth-Science Reviews, 181, 12–42.Google Scholar
Krmíček, L., Magna, T., Pandey, A., Rao, N.C. and Kynický, J. (2022) Lithium isotopes in kimberlites, lamproites and lamprophyres as tracers of source components and processes related to supercontinent cycles. Geological Society, London, Special Publications, 513, 209–236.CrossRefGoogle 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.CrossRefGoogle Scholar
Kumar, A., Parashuramulu, V. and Nagaraju, E. (2015) A 2082 Ma radiating dyke swarm in the Eastern Dharwar Craton, southern India and its implications to Cuddapah basin formation. Precambrian Research, 266, 490–505.CrossRefGoogle Scholar
Kumar, S.P., Shaikh, A.M., Patel, S.C., Sheikh, J.M., Behera, D., Pruseth, K.L., Ravi, S. and Tappe, S. (2021) Multi-stage magmatic history of olivine–leucite lamproite dykes from Banganapalle, Dharwar craton, India: evidence from compositional zoning of spinel. Mineralogy and Petrology, 115, 87–112.CrossRefGoogle 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.CrossRefGoogle Scholar
Locock, A.J. (2014) An Excel spreadsheet to classify chemical analyses of amphiboles following the IMA 2012 recommendations. Computers & Geosciences, 62, 1–11.CrossRefGoogle Scholar
Mitchell, R.H. (1985) A review of the mineralogy of lamproites. Transactions of the Geological Society of South Africa, 88, 411–437.Google Scholar
Mitchell, R.H. (1986) Kimberlites: Mineralogy, Geochemistry and Petrology. Plenum Press, New York, 978pp.CrossRefGoogle Scholar
Mitchell, R.H. (1994) The lamprophyre facies. Mineralogy and Petrology, 51(2–4), 137–146.CrossRefGoogle Scholar
Mitchell, R.H. (1995) Kimberlites, Orangeites, and Related Rocks. Plenum Press, New York, 410pp.CrossRefGoogle Scholar
Mitchell, R.H. (2020a) Potassic alkaline rocks: leucitites, lamproites, and kimberlites. In: Reference Module in Earth Systems and Environmental Sciences, 1–25, doi: 10.1016/B978-0-12-409548-9.12482-0CrossRefGoogle Scholar
Mitchell, R.H. (2020b) Igneous rock associations 26. Lamproites, exotic potassic alkaline rocks: a review of their nomenclature, characterization and origins. Geoscience Canada: Journal of the Geological Association of Canada/Geoscience Canada: journal de l'Association Géologique du Canada, 47, 119–142.Google Scholar
Mitchell, R.H. and Bergman, S.C. (1991) Petrology of Lamproites. Plenum Press, New York, 447pp.CrossRefGoogle 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
Naqvi, S.M. and Rogers, J.J.W. (1987) Precambrian Geology of India. Oxford monographs on Geology and Geophysics No. 6. Oxford University Press, Oxford, UK, 223pp.Google Scholar
Ngwenya, N.S. and Tappe, S. (2021) Diamondiferous lamproites of the Luangwa Rift in central Africa and links to remobilized cratonic lithosphere. Chemical Geology, 568, 120019.CrossRefGoogle Scholar
Pandey, A. and Chalapathi Rao, N.V. (2020) Supercontinent transition as a trigger for ~1.1 Gyr diamondiferous kimberlites and related magmatism in India. Lithos, 370–371, 105620, https://doi.org/10.1016/j.lithos.2020.105620CrossRefGoogle Scholar
Prelević, D., Foley, S.F., Romer, R. and Conticelli, S. (2008) Mediterranean Tertiary lamproites derived from multiple source components in postcollisional geodynamics. Geochimica et Cosmochimica Acta, 72, 2125–2156.CrossRefGoogle Scholar
Ramakrishnan, M. and Vaidyanadhan, R. (2008) Geology of India, vol. I & II. Geological Society of India, Bangalore.Google Scholar
Ravi, S., Sufija, M.V., Patel, S.C., Sheikh, J.M., Sridhar, M., Kaminsky, F.V., Khachatryan, G.K., Nayak, S.S. and Bhaskara Rao, K.S. (2013) Diamond potential of the Eastern Dharwar Craton, southern India, and a reconnaissance study of physical and infrared characteristics of the diamonds. Pp. 335–348 in: Proceedings of 10th International Kimberlite Conference. Springer, New Delhi.CrossRefGoogle Scholar
Rieder, M., Cavazzini, D., Yakonov, Y.S.D., Frank-Kamenetskii, V.A., Gottardi, G., Guggenheim, S., Koval, P.V., Muller, G., Neiva, A.M.R., Radoslovich, E.W., Robert, J.L., Sassi, F.P., Takeda, H., Weiss, Z. and Wones, D.R. (1998) Nomenclature of the micas. The Canadian Mineralogist, 36, 905–912.Google Scholar
Scott Smith, B.H. and Skinner, E.M.W. (1984) Diamondiferous lamproites. Journal of Geology, 92, 433–438.CrossRefGoogle Scholar
Scott Smith, B.H., Nowicki, T.E., Russell, J.K., Webb, K.J., Mitchell, R.H., Hetman, C.M. and Robey, J.V. (2018) A Glossary of Kimberlite and Related Terms Part 1: Glossary. Scott-Smith Petrology Inc., North Vancouver, British Columbia, Canada, 144 pp.Google Scholar
Shaikh, A.M., Patel, S.C., Ravi, S., Behera, D. and Pruseth, K.L. (2017) Mineralogy of the TK1 and TK4 ‘kimberlites’ 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.CrossRefGoogle 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, 112, 609–624.Google Scholar
Shaikh, A.M., Patel, S.C., Bussweiler, Y., Kumar, S.P., Tappe, S., Ravi, S. and Mainkar, D. (2019) Olivine trace element compositions in diamondiferous lamproites from India: Proxies for magma origins and the nature of the lithospheric mantle beneath the Bastar and Dharwar cratons. Lithos, 324, 501–518.CrossRefGoogle Scholar
Sridhar, M. and Rau, T.K. (2005) Discovery of a new lamproite field—Ramadugu lamproite field (RLF), Nalgonda District, Andhra Pradesh. Pp. 55–57 in: Proceedings of the Group Discussion on Kimberlites and Related Rocks of India. Organized by the Geological Society of India, Bangalore, India [Extended abstracts].Google Scholar
Srivastava, R.K., Samal, A.K. and Gautam, G.C. (2015) Geochemical characteristics and petrogenesis of four Palaeoproterozoic mafic dike swarms and associated large igneous provinces from the eastern Dharwar craton, India. International Geology Review, 57(11–12), 1462–1484.CrossRefGoogle Scholar
Swaminath, J. and Ramakrishnan, M. (1981) Early Precambrian Supracrustals of Southern Karnataka. Memoirs of Geological Survey of India, 112, 350.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. Mineralogy and Petrology, 173, 67.CrossRefGoogle Scholar
Tappe, S., Foley, S.F., Jenner, G.A. and Kjarsgaard, B.A. (2005) Integrating ultramafic lamprophyres into the IUGS classification of igneous rocks: rationale and implications. Journal of Petrology, 46, 1893–1900.CrossRefGoogle Scholar
Woolley, A.R., Bergman, S.C., Edgar, A.D., Le Bas, M.J., Mitchell, R.H., Rock, N.M.S. and Scott Smith, B.H. (1996) Classification of lamprophyres, lamproites, kimberlites, and the kalsilite-, melilite and leucite-bearing rocks. Canadian Mineralogist, 34, 175–186.Google Scholar