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Palaeomagnetism of the uppermost carbonate units of the Purana basins in southern India: new demagnetization results from the Kaladgi and Bhima basins, Karnataka

Published online by Cambridge University Press:  19 November 2020

Herve Wabo Open the ORCID record for Herve Wabo [Opens in a new window] ,
Michiel Olivier De Kock ,
Nicolas Johannes Beukes  and
Venkatraman Seetaram Hegde
Herve Wabo*
Affiliation:
Department of Science and Innovation, National Research Foundation, Centre of Excellence for Integrated Mineral and Energy Resource Analysis (DSI-NRF CIMERA) and Paleoproterozoic Mineralization Research Group (PPM Research Group), Department of Geology, University of Johannesburg, PO Box 524, Auckland Park 2006, Johannesburg, South Africa
Michiel Olivier De Kock
Affiliation:
Department of Science and Innovation, National Research Foundation, Centre of Excellence for Integrated Mineral and Energy Resource Analysis (DSI-NRF CIMERA) and Paleoproterozoic Mineralization Research Group (PPM Research Group), Department of Geology, University of Johannesburg, PO Box 524, Auckland Park 2006, Johannesburg, South Africa
Nicolas Johannes Beukes
Affiliation:
Department of Science and Innovation, National Research Foundation, Centre of Excellence for Integrated Mineral and Energy Resource Analysis (DSI-NRF CIMERA) and Paleoproterozoic Mineralization Research Group (PPM Research Group), Department of Geology, University of Johannesburg, PO Box 524, Auckland Park 2006, Johannesburg, South Africa
Venkatraman Seetaram Hegde
Affiliation:
Civil Engineering Department, Sri Dharmasthala Manjunatheshwara (SDM) College of Engineering and Technology, Dharwar580 002, Karnataka, India
*
Author for correspondence: Herve Wabo, Email: [email protected]
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Abstract

Four unconformity-bound sequences can be identified in the Purana successions in southern India, of which the third sequence (Sequence III) has the widest distribution. Sequence III contains deep-water carbonate units with consistent sedimentological characteristics across the subcontinent. The current extent of field relationships and existing ages has not allowed the correlation and chronology of these carbonates to be established conclusively. Palaeomagnetism may help resolve this essential question for the Purana sedimentation. Here, we report new palaeomagnetic results (HIG+/– pole: 21.7° N, 81.1° E, radius of cone of 95% confidence A95 = 15.9°) from Sequence III carbonates in the Kaladgi (Badami Group) and Bhima (Bhima Group) basins. The HIG+/– magnetization, revealed after the removal of secondary magnetizations that include a present-day field and an Ediacaran–Cambrian overprint, is interpreted to be primary based on its dissimilarity to known younger magnetizations, the presence of distinctly different magnetic components in sites and a positive reversal test. Our HIG+/– pole differs from the c. 1.4 Ga pole and various c. 1.1 Ga and younger poles. Instead, it overlaps with the Harohalli dyke pole that was long considered to be c. 823 Ma in age, but has recently been suggested to be much older with an age of c. 1192 Ma. We therefore consider the uppermost carbonate beds of Badami and Bhima groups to have been deposited during late Mesoproterozoic times. A critical evaluation of parameters from which an earlier Neoproterozoic age for these carbonates was established indicates that the available 40Ar/39Ar, Rb–Sr and U–Pb ages in the Kaladgi and Bhima basins could reflect the timing of post-depositional alteration events.

Keywords

southern IndiaPurana basinsunconformity-bound Sequence IIIcarbonatespalaeomagnetism
Type
Original Article
Information
Geological Magazine , Volume 159 , Issue 2: Mesoproterozoic Basins recording Earth’s Middle Age , February 2022 , pp. 269 - 278
Copyright
© The Author(s), 2020. Published by Cambridge University Press

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References

Bates, PM and Jones, DL (1996) A palaeomagnetic investigation of the Mashonaland dolerites, north-east Zimbabwe. Geophysical Journal International 126, 513–24.CrossRefGoogle Scholar
Belica, ME, Piispa, EJ, Meert, JG, Pesonen, L, Plado, J, Manoj, J, Pandit, K, Kamenov, GD and Celestino, M (2014) Paleoproterozoic mafic dyke swarms from the Dharwar craton; paleomagnetic poles for India from 2.37 to 1.88 Ga and rethinking the Columbia supercontinent. Precambrian Research 244, 100–22.CrossRefGoogle Scholar
Bernard-Griffiths, JB (1989) The rubidium-strontium method. In Nuclear 327 Methods of Dating (eds Roth, E and Poty, B), pp. 73–94. New York: Kluwer Academic Publishers.Google Scholar
Bickford, ME, Basu, A, Patranabis-Deb, S, Dhang, PC and Schieber, J (2011) Depositional history of the Chattisgarth Basin, Central India: constraints from new SHRIMP zircon ages. The Journal of Geology 119, 33–50.CrossRefGoogle Scholar
Bohnel, H (1999) Paleomagnetic study of Jurassic and Cretaceous rocks from the Mixteca terrane (Mexico). Journal of South American Earth Sciences 12, 545–56.CrossRefGoogle Scholar
Chakraborty, PP, Dey, S and Mohanty, SP (2010) Proterozoic platform sequences of Peninsular India: implications towards basin evolution and supercontinent assembly. Journal of Asian Earth Sciences 39, 589–607.CrossRefGoogle Scholar
Chalapathi Rao, NV, Anand, M, Dongre, A and Osborne, I (2010) Carbonate xenoliths hosted by the Mesoproterozoic Siddanpalli Kimberlite Cluster (Eastern Dharwar craton): implications for the geodynamic evolution of southern India and its diamond and uranium metallogenesis. International Journal of Earth Sciences 99, 1791–804.CrossRefGoogle Scholar
Chatterjee, N and Ghose, NC (2001) Extensive early Neoproterozoic high-grade metamorphism in North Chotanagpur Gneissic Complex of the Central IndianTectonic Zone. Gondwana Research 20, 362–79.CrossRefGoogle Scholar
Chaudhuri, AK, Mukhopadhyay, J, Patranabis-Deb, S and Chanda, SK (1999) The Neoproterozoic successions of peninsular India. Gondwana Research 2, 213–25.CrossRefGoogle Scholar
Chaudhuri, AK, Saha, D, Deb, GK, Patranabis-Deb, S, Mukherjee, MK and Gosh, G (2002) The Purana basins of southern cratonic province of India: a case for Mesoproterozoic fossil rifts. Gondwana Research 5, 23–33.CrossRefGoogle Scholar
Collins, AS, Patranabis-Deb, S, Alexander, E, Bertram, CN, Falster, GM, Gore, RJ, Mackintosh, J, Dhang, PC, Saha, D, Payne, JL, Jourdan, F, Backé, G, Halverson, GP and Wade, BP (2015) Detrital mineral age, radiogenic isotopic stratigraphy and tectonic significance of the Cuddapah Basin, India. Gondwana Research 28, 1294–309.CrossRefGoogle Scholar
Conrad, JE, Hein, JR, Chaudhuri, AK, Patranabis-Deb, S, Mukhopadhyay, J, Deb, GK and Beukes, NJ (2011) Constraints on the development of central India Proterozoic basins from 40Ar/39Ar analysis of authigenic glauconitic minerals. GSA Bulletin 123, 158–67.CrossRefGoogle Scholar
Crawford, AR and Compston, W (1973) The age of the Cuddapah and Kurnool systems, southern India. Journal of the Geological Society of Australia 19, 453–64.CrossRefGoogle Scholar
De Kock, MO, Beukes, NJ and Mukhopadhyay, J (2015) Palaeomagnetism of Mesoproterozoic limestone and shale successions of some Purana basins in southern India. Geological Magazine 152, 728–50.CrossRefGoogle Scholar
Dey, S (2015) Geological history of the Kaladgi–Badami and Bhima basins, south India: Sedimentation in a Proterozoic intracratonic setup. In Precambrian Basins of India: Stratigraphic and Tectonic Context (eds Mazumder, R and Eriksson, PG), pp. 283–96. Geological Society of London, Memoir no. 43.Google Scholar
Dongre, A, Chalapathi Rao, NV and Kamde, G (2008) Limestone xenolith in Siddanpalli Kimberlite, Gadwal granite-greenstone terrain, eastern Dharwar craton, Southern India: remnant of Proterozoic platformal cover sequence of Bhima/Kurnool Age? Journal of Geology 116, 184–91.CrossRefGoogle Scholar
Evans, DAD, Beukes, NJ and Kirschvink, JL (2002) Paleomagnetism of a lateritic paleoweathering horizon and overlying Paleoproterozoic red beds from South Africa: Implications for the Kaapvaal apparent polar wander path and a confirmation of atmospheric oxygen enrichment. Journal of Geophysical Research 107, 2326–33.CrossRefGoogle Scholar
Fisher, RA (1953) Dispersion on a sphere. Proceedings of the Royal Society of London. Series A 217, 295–305.CrossRefGoogle Scholar
Goutham, MR, Raghubabu, K, Prasad, CVRK, Subba Rao, KV and Damodara Reddy, V (2006) A Neoproterozoic geomagnetic field reversal from the Kurnool Group, India: implications for stratigraphic correlation and formation of Gondwanaland. Journal Geological Society of India 67, 221–33.Google Scholar
Gregory, LC, Meert, JG, Pradhan, V, Pandit, MK, Tamrat, E and Malone, SJ (2006) A paleomagnetic and geochronologic study of the Majhgawan kimberlite, India: implications for the age of the Upper Vindhyan Supergroup. Precambrian Research 149, 65–75.CrossRefGoogle Scholar
Halls, HC, Kumar, A, Srinivasan, R and Hamilton, MA (2007) Paleomagnetism and U-Pb geochronology of easterly trending dykes in the Dharwar craton, India: feldspar clouding, radiating dyke swarms and the position of India at 2.37 Ga. Precambrian Research 155, 47–68.CrossRefGoogle Scholar
Humbert, F, Sonnette, L, De Kock, MO, Robion, P, Horng, CS, Cousture, A and Wabo, H (2017) Palaeomagnetism of the early Palaeoproterozoic, volcanic Hekpoort Formation (Transvaal Supergroup) of the Kaapvaal craton, South Africa. Geophysical Journal International 209, 842–65.CrossRefGoogle Scholar
Ikramuddin, M and Stueber, AM (1976) Rb-Sr ages of Precambrian dolerite and alkaline dykes, south-east Mysore State, India. Lithos 9, 235–241.CrossRefGoogle Scholar
Jones, CH (2002) User-driven integrated software lives: “Paleomag” paleomagnetic analysis on the MacintoshTM. Computers and Geosciences 28, 1145–51.CrossRefGoogle Scholar
Joy, S, Patranabis-Deb, S, Saha, D, Jelsma, H, Maas, R, Söderlund, U, Tappe, S, Gert Van Der Linde, G, Banerjee, A and Krishnan, U (2018) Depositional history and provenance of cratonic “Purana” basins in southern India: a multipronged geochronology approach to the Proterozoic Kaladgi and Bhima basins. Geological Journal 54, 2957–79,  doi: 10.1002/gj.3415.CrossRefGoogle Scholar
Kale, VS and Phansalkar, VG (1991) Purana basins of peninsular India: a review. Basin Research 3, 1–36.CrossRefGoogle Scholar
Kirschvink, JL (1980) The least-squares line and plane and the analysis of palaeomagnetic data. Geophysical Journal of the Royal Astronomical Society 62, 699–718.CrossRefGoogle Scholar
Kirschvink, JL, Kopp, RE, Raub, TD, Baumgartner, CT and Holt, JW (2008) Rapid, precise, and high-sensitivity acquisition of paleomagnetic and rockmagentic data: development of a low-noise automatic sample changing system for superconducting rock magnetometers. Geochemistry, Geophysics and Geosystems 9, Q05Y01, doi: 10.1029/2007GC001856.CrossRefGoogle Scholar
Kumar, A, Sivaraman, TV, Bhaskararao, YJ and Gopalan, K (1989) Rb-Sr ages of two dyke swarms from the Dharwar craton, Karnataka (abstract). In Nuclear Methods of Dating (eds Roth, E and Poty, B), pp. 73–104. Netherlands: CEA.Google Scholar
Letts, S, Torsvik, TH, Webb, SJ and Ashwal, LD (eds) (2010) New Palaeoproterozoic palaeomagnetic data from the Kaapvaal Craton. In The Formation and Evolution of Africa: A Synopsis of 3.8 Ga of Earth History (eds DJJ van Hinsbergen, SJH Buiter, TH Torsvik, C Gaina and SJ Webb), pp. 9–26. Geological Society of London, Special Publication no. 357.Google Scholar
Li, Z, Evans, D and Zhang, S (2004) A 90° spin on Rodinia: Possible causal links between the Neoproterozoic supercontinent, superplume, true polar wander and low-latitude glaciation. Earth and Planetary Science Letters 220, 409–21.CrossRefGoogle Scholar
Malone, SJ, Meert, JG, Banerjee, S, Pandit, MK, Tamrat, E, Kamenov, GD, Pradhan, VR and Sohl, LE (2008) Paleomagnetism and detrital zircon geochronology of the Upper Vindhyan sequence, Son Valley and Rajastan, India: A ca. 1000 Ma closure age for the Purana basins? Precambrian Research 164, 137–59.CrossRefGoogle Scholar
Maloof, AC, Havlorsen, GP, Kirschvink, JL, Schrag, DP, Weiss, BP and Hoffman, PF (2006) Combined paleomagnetic, isotopic, and stratigraphic evidence for true polar wander from the Neoproterozoic Akademikerbreen Group, Svalbard, Norway. Geological Society of America Bulletin 118, 1099–124.CrossRefGoogle Scholar
McFadden, PL and McElhinny, MW (1990) Classification of the reversal test in palaeomagnetism. Geophysical Journal International 103, 725–29.CrossRefGoogle Scholar
Meert, JG and Pandit, MK (2015) The Archaean and Proterozoic history of Peninsular India: tectonic framework for Precambrian sedimentary basins in India. In Precambrian Basins of India: Stratigraphic and Tectonic Context (eds Mazumder, R and Eriksson, PG), pp. 29–54. Geological Society of London, Memoir no. 43.Google Scholar
Mukhopadhyay, J and Chaudhuri, AK (2003) Stratigraphy of the Chanda Limestone from the Proterozoic Penganga Group, Adilabad, Andhra Pradesh, India: Implications for understanding depositional setting and palaeogeography. Journal of the Geological Society of India 62, 356–68.Google Scholar
Patil Pillai, S, Pande, K and Kale, VS (2018) Implications of new 40Ar/39Ar age of Mallapur Intrusives on the chronology and evolution of the Kaladgi Basin, Dharwar Craton. Journal of Earth System Science 127, 32, doi: 10.1007/s12040-018-0940-5.Google Scholar
Patranabis-Deb, S, Bickford, ME, Hill, B, Chaudhuri, AK and Basu, A (2007) SHRIMP ages of zircon in the uppermost tuff in Chattisgarh Basin in Central India require 500 Ma adjustment in Indian Proterozoic Stratigraphy. The Journal of Geology 115, 407–15.CrossRefGoogle Scholar
Patranabis-Deb, S, Saha, D and Tripathy, V (2012) Basin stratigraphy, sea-level fluctuations and their global tectonic connections: evidence from the Proterozoic Cuddapah Basin. Geological Journal 47, 263–83.CrossRefGoogle Scholar
Pisarevsky, SA, Biswal, TK, Wang, XC, Dewaele, B, Ernst, RE, Söderlund, U, Tait, JA, Ratre, K, Singh, YK and Cleve, M (2013) Palaeomagnetic, geochronological and geochemical study of Mesoproterozoic Lakhna Dykes in the Bastar Craton, India: implications for the Meosproterozoic supercontinent. Lithos 174, 125–43.CrossRefGoogle Scholar
Pivarunas, AF, Meert, JG, Pandit, MK and Sinha, A (2019) Paleomagnetism and geochronology of mafic dykes from the Southern Granulite Terrane, India: Expanding the Dharwar craton southward. Tectonophysics 760, 4–22.CrossRefGoogle Scholar
Pradhan, VR, Meert, JG, Pandit, MK, Kamenov, G and Mondal, MEA (2012) Paleomagnetic and geochronological studies of the mafic dyke swarms of Bundelkhand craton, central India: Implications for the tectonic evolution and paleogeographic reconstructions. Precambrian Research 198–199, 51–76.CrossRefGoogle Scholar
Pradhan, VR, Pandit, MK and Meert, JG (2008) A cautionary note on the age of the paleomagnetic pole obtained from the Harohalli dyke swarms, Dharwar craton, southern India. In Indian Dykes (eds Srivastava, RK, Sivaji, C and Rao, NVC), pp. 339–52. New Delhi, India: Narosa Publishing House.Google Scholar
Radhakrishna, T and Joseph, M (1996) Late Precambrian (850-800 Ma) paleomagnetic pole for the south Indian shield from the Harohalli alkaline dykes: geotectonic implications for Gondwana reconstructions. Precambrian Research 80, 77–87.CrossRefGoogle Scholar
Saha, D, Patranabis-Deb, S and Collins, AS (2016) Proterozoic stratigraphic of Southern India cratons and global context. In Stratigraphy and Timescales (ed. Montenari, M), Volume 1, pp. 1–59. Amsterdam: Elsevier.Google Scholar
Van Der Voo, R (1990) The reliability of paleomagnetic data. Tectonophysics 184, 1–9.CrossRefGoogle Scholar
Williams, S, Müller, RD, Landgrebe, TCW and Whittaker, JM (2012) An open-source software environment for visualizing and refining plate tectonic reconstructions using high resolution geological and geophysical data sets. GSA Today 22(4–5), doi: 10.1130/GSATG139A.CrossRefGoogle Scholar