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Metamorphic evolution of the Sittampundi Layered Complex, India, during the Archaean–Proterozoic boundary: insight from pseudosection modelling and zircon U–Pb SHRIMP geochronology
Published online by Cambridge University Press: 26 May 2022
Abstract
In the Palghat–Cauvery Shear/Suture Zone of the Southern Granulite Terrane, the Sittampundi Layered Complex occurs as a mappable unit. The Sittampundi Layered Complex consists of mafic, ultramafic and anorthositic rocks with chromitite layers and has been interpreted as an arc/ophiolite complex that formed in an Archaean suprasubduction zone arc setting. In the Sittampundi Layered Complex, reddish-black metabasites occur as layers or boudins with a rim of amphibolite within anorthosite. The peak metamorphic assemblage of the metabasites is garnet + clinopyroxene + quartz + rutile ± plagioclase ± orthopyroxene, and symplectite consisting of amphibole and plagioclase formed around the garnet during retrograde metamorphism. The protolith of metabasite may have intruded in a suprasubduction zone arc setting during the late Neoarchaean (c. 2540–2520 Ma), and then underwent high-pressure granulite-facies peak metamorphism (900–800 °C and 11–14 kbar) in the early Palaeoproterozoic (c. 2460–2440 Ma), followed by amphibolite-facies metamorphism (550–480 °C and 5.5–4.5 kbar) in the middle Palaeoproterozoic (c. 1900–1850 Ma). The results obtained in this study, together with previous studies, indicate that: (1) the high-pressure granulite-facies metamorphism in the study area indicates that subduction occurred during the Archaean–Proterozoic boundary with a higher apparent average geothermal gradient (∼20–16 °C km−1) than the modern-day Earth, and (2) the apparent average geothermal gradient of the subduction zone was ∼29–14 °C km−1 during the Archaean–Proterozoic boundary, which was still too high to enter the realm of eclogite-facies metamorphism.
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References
Ague, JJ and Eckert, JO (2012) Precipitation of rutile and ilmenite needles in garnet: implications for extreme metamorphic conditions in the Acadian Orogen, U.S.A. American Mineralogist 97, 840–55. doi: 10.2138/am.2012.4015.CrossRefGoogle Scholar
Ai, Y (1994) A revision of the garnet-clinopyroxene Fe2+-Mg exchange geothermometer. Contributions to Mineralogy and Petrology 115, 467–73. doi: 10.1007/BF00320979.CrossRefGoogle Scholar
Alabaster, T, Pearce, JA and Malpas, J (1982) The volcanic stratigraphy and petrogenesis of the Oman ophiolite complex. Contributions to Mineralogy and Petrology 81, 168–83.CrossRefGoogle Scholar
Amaldev, T, Santosh, M, Tang, L, Baiju, KR, Tsunogae, T and Satyanarayanan, M (2016) Mesoarchean convergent margin processes and crustal evolution: petrologic, geochemical and zircon U–Pb and Lu–Hf data from the Mercara Suture Zone, southern India. Gondwana Research 37, 182–204. doi: 10.1016/j.gr.2016.05.017.CrossRefGoogle Scholar
Anderson, JR, Payne, JL, Kelsey, DE, Hand, M, Collins, AS and Santosh, M (2012) High-pressure granulites at the dawn of the Proterozoic. Geology 40, 431–4. doi: 10.1130/G32854.1.CrossRefGoogle Scholar
Behera, BM, Waele, BD, Thirukumaran, V, Sundaralingam, K, Narayanan, S, Sivalingam, B and Biswal, TK (2019) Kinematics, strain pattern and geochronology of the Salem-Attur shear zone: tectonic implications for the multiple sheared Salem-Namakkal blocks of the Southern Granulite terrane, India. Precambrian Research 324, 32–61. doi: 10.1016/j.precamres.2019.01.022.CrossRefGoogle Scholar
Bhaskar Rao, YJ, Janardhan, AS, Vijaya Kumar, T, Narayana, BL, Dayal, AM, Taylor, PN and Chetty, TRK (2003) Sm-Nd model ages and Rb-Sr isotope systematics of charnockites and gneisses across the Cauvery shear zone, southern India: implications for the Archaean–Neoproterozoic boundary in the southern granulite terrain. In Tectonics of Southern Granulite Terrain (ed. Ramakrishnan, M), pp. 297–317. Geological Society of India Memoir, 50.Google Scholar
Bhattacharya, A, Krishnakumar, KR, Raith, M and Sen, SK (1991) An improved set of a-X parameters for Fe-Mg-Ca garnets and refinements of the orthopyroxene-garnet thermometer and the orthopyroxene-garnet-plagioclase-quartz barometer. Journal of Petrology 32, 629–56. doi: 10.1093/petrology/32.3.629.CrossRefGoogle Scholar
Brandt, S, Raith, MM, Schenk, V, Sengupta, P, Srikantappa, C and Gerdes, A (2014) Crustal evolution of the Southern Granulite Terrane, south India: new geochronological and geochemical data for felsic orthogneisses and granites. Precambrian Research 246, 91–122. doi: 10.1016/j.precamres.2014.01.007.CrossRefGoogle Scholar
Braun, I and Kriegsman, LM (2003) Proterozoic crustal evolution of southernmost India and Sri Lanka. In Proterozoic East Gondwana: Supercontinent Assembly and Breakup (eds Yoshida, M, Windley, B and Dasgupta, S), pp. 169–202. Geological Society of London, Special Publication no. 206.Google Scholar
Brown, M (2006) Duality of thermal regimes is the distinctive characteristic of plate tectonics since the Neoarchean. Geology 34, 961–4. doi: 10.1130/g22853a.1.CrossRefGoogle Scholar
Brown, M (2007) Metamorphic conditions in orogenic belts: a record of secular change. International Geology Review 49, 193–234. doi: 10.2747/0020-6814.49.3.193.CrossRefGoogle Scholar
Brown, M (2010) Paired metamorphic belts revisited. Gondwana Research 18, 46–59. doi: 10.1016/j.gr.2009.11.004.CrossRefGoogle Scholar
Brown, M (2014) The contribution of metamorphic petrology to understanding lithosphere evolution and geodynamics. Geoscience Frontiers 5, 553–69. doi: 10.1016/j.gsf.2014.02.005.CrossRefGoogle Scholar
Brown, M and Johnson, T (2018) Secular change in metamorphism and the onset of global plate tectonics. American Mineralogist 103, 181–96. doi: 10.2138/am-2018-6166.CrossRefGoogle Scholar
Brown, M and Johnson, T (2019) Time’s arrow, time’s cycle: granulite metamorphism and geodynamics. Mineralogical Magazine 83, 323–38. doi: 10.1180/mgm.2019.19.CrossRefGoogle Scholar
Brown, M, Johnson, T and Gardiner, NJ (2020a) Plate tectonics and the Archean earth. Annual Reviews of Earth and Planetary Sciences 48, 291–320. doi: 10.1146/annurev-earth-081619-052705.CrossRefGoogle Scholar
Brown, M, Kirkland, CL and Johnson, TE (2020b) Evolution of geodynamics since the Archean: significant change at the dawn of the Phanerozoic. Geology 48, 488–92. doi: 10.1130/G47417.1.CrossRefGoogle Scholar
Cawood, PA, Hawkesworth, CJ, Pisarevsky, SA, Dhuime, B, Capitanio, FA and Nebel, O (2018) Geological archive of the onset of plate tectonics. Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 376, 20170405. doi: 10.1098/rsta.2017.0405.CrossRefGoogle ScholarPubMed
Cawood, PA, Kröner, A and Pisarevsky, S (2006) Precambrian plate tectonics: criteria and evidence. GSA Today 16, 4–11. doi: 10.1130/GSAT01607.1.CrossRefGoogle Scholar
Chattopadhyay, A, Bhowmik, SK and Roy, A (2020) Tectonothermal evolution of the Central Indian Tectonic Zone and its implications for Proterozoic supercontinent assembly: the current status. Episodes 43, 132–44. doi: 10.18814/epiiugs/2020/020008.CrossRefGoogle Scholar
Chen, NH-C, Zhao, G, Jahn, B-M, Sun, M and Zhou, H (2017a) U-Pb zircon ages and Hf isotopes of ∼2.5 Ga granitoids from the Yinshan Block, North China Craton: implications for crustal growth. Precambrian Research 303, 171–82.CrossRefGoogle Scholar
Chen, Y, Zhang, Z, Li, K, Li, Q and Luo, Z (2017b) Provenance of the Middle Permian Zhesi Formation in central Inner Mongolia, northern China: constraints from petrography, geochemistry and detrital zircon U–Pb geochronology. Geological Journal 52, 92–109. doi: 10.1002/gj.2735.CrossRefGoogle Scholar
Chetty, TRK and Bhaskar Rao, YJ (2006) The Cauvery shear zone, Southern Granulite Terrain, India: a crustal-scale flower structure. Gondwana Research 10, 77–85.CrossRefGoogle Scholar
Chetty, TRK, Bhaskar Rao, YJ and Narayana, BL (2003) A structural cross-section along Krishnagiri-Palani corridor, southern granulite terrain India. In Tectonics of Southern Granulite Terrain, Kuppam-Palani Geotransect (ed Ramakrishnan, M), pp. 255–77. Geological Society of India Memoir, 50.Google Scholar
Chetty, TRK (1996) Proterozoic shear zones in southern granulite terrain, India. In The Archean and Proterozoic Terrain of Southern India within Gondwana (eds Santosh, M and Yoshida, M), pp. 77–89. Gondwana Research Group Memoirs 3, Field Science Publications.Google Scholar
Chowdhury, P and Chakraborty, S (2019) Slow cooling at higher temperatures recorded within high-P mafic granulites from the Southern Granulite Terrain, India: implications for the presence and style of plate tectonics near the Archean-Proterozoic boundary. Journal of Petrology 60, 441–85. doi: 10.1093/petrology/egz001.CrossRefGoogle Scholar
Chowdhury, P, Talukdar, M, Sengupta, P, Sanyal, S and Mukhopadhyay, D (2013) Controls of P-T path and element mobility on the formation of corundum pseudomorphs in Paleoproterozoic high-pressure anorthosite from Sittampundi, Tamil Nadu, India. American Mineralogist 98, 1725–37. doi: 10.2138/am.2013.4350.CrossRefGoogle Scholar
Claoue-Long, JC, Compston, W, Roberts, J and Fanning, CM (1995) Two Carboniferous ages: a comparison of SHRIMP zircon dating with conventional zircon ages and 40Ar/39Ar analysis. In Geochronology Time Scales and Global Stratigraphic Correlation (eds Berggren, WA, Kent, DV, Aubry, MP and Hardenbol, J), pp. 3–21. SEPM (Society for Sedimentary Geology) Special Publication 4.Google Scholar
Clark, C, Collins, AS, Kinny, PD, Timms, NE and Chetty, TRK (2009) SHRIMP U-Pb age constraints on the age of charnockite magmatism and metamorphism in the Salem Block, southern India. Gondwana Research 16, 27–36.CrossRefGoogle Scholar
Clark, C, Healy, D, Johnson, T, Collins, AS, Taylor, RJ, Santosh, M and Timms, NE (2015) Hot orogens and supercontinent amalgamation: a Gondwanan example from southern India. Gondwana Research 28, 1310–28.CrossRefGoogle Scholar
Collins, AS, Clark, C and Plavsa, D (2014) Peninsular India in Gondwana: tectonothermal evolution of the Southern Granulite Terrane and its Gondwanan counterparts. Gondwana Research 25, 190–203.CrossRefGoogle Scholar
Collins, AS, Clark, C, Sajeev, K, Santosh, M, Kelsey David, E and Matin, H (2007a) Passage through India: Mozambique Ocean suture, high pressure granulites and Palghat-Cauvery shear zone system. Terra Nova 19, 41–7.CrossRefGoogle Scholar
Collins, AS, Santosh, M, Braun, I and Clark, C (2007b) Age and sedimentary provenance of the Southern Granulites, South India: U-Th-Pb SHRIMP secondary ion mass spectrometry. Precambrian Research 155, 125–38. doi: 10.1016/j.precamres.2007.01.006.CrossRefGoogle Scholar
Compston, W (1999) Geological age by instrumental analysis: the 29th Hallimond lecture. Mineralogical Magazine 63, 297–311.CrossRefGoogle Scholar
Condie, K (2021) Two major transitions in earth history: evidence for two lithospheric strength thresholds. The Journal of Geology 129, 455–73.CrossRefGoogle Scholar
Connolly, JAD and Petrini, K (2002) An automated strategy for calculation of phase diagram sections and retrieval of rock properties as a function of physical conditions (0.4 Mb). Journal of Metamorphic Geology 20, 697–708.CrossRefGoogle Scholar
Corfu, F, Hanchar, JM, Hoskin, PWO and Kinny, P (2003) Atlas of zircon textures. Reviews in Mineralogy and Geochemistry 53, 469–500. doi: 10.2113/0530469.CrossRefGoogle Scholar
Dale, J, Holland, T and Powell, R (2000) Hornblende-garnet-plagioclase thermobarometry: a natural assemblage calibration of the thermodynamics of hornblende. Contributions to Mineralogy and Petrology 140, 353–62.CrossRefGoogle Scholar
Dasgupta, S, Bose, S and Das, K (2013) Tectonic evolution of the Eastern Ghats Belt, India. Precambrian Research 227, 247–58.CrossRefGoogle Scholar
Dey, A, Karmakar, S, Ibanez-Mejia, M, Mukherjee, S, Sanyal, S and Sengupta, P (2020) Petrology and geochronology of a suite of pelitic granulites from parts of the Chotanagpur Granite Gneiss Complex, eastern India: evidence for Stenian-Tonian reworking of a late Paleoproterozoic crust. Geological Journal 55, 2851–80. doi: 10.1002/gj.3552.CrossRefGoogle Scholar
Dharma Rao, CV, Santosh, M, Sajeev, K and Windley, BF (2012) Chromite–silicate chemistry of the Neoarchean Sittampundi Complex, southern India: implications for subduction-related arc magmatism. Precambrian Research 227, 259–75.CrossRefGoogle Scholar
Droop, GTR (1987) A general equation for estimating Fe3+ concentrations in ferromagnesian silicates and oxides from microprobe analyses, using stoichiometric criteria. Geological Magazine 51, 431–5.Google Scholar
Drury, SA, Harris, NBW, Holt, RW, Reeves-Smith, GJ and Wightman, RT (1984) Precambrian tectonics and crustal evolution in South India. Journal of Geology 92, 3–20.CrossRefGoogle Scholar
Drury, SA and Holt, RW (1980) The tectonic framework of the South Indian craton: a reconnaissance involving LANDSAT imagery. Tectonophysics 65, 1–15.CrossRefGoogle Scholar
Dutta, U, Bhui, UK, Sengupta, P, Sanyal, S and Mukhopadhyay, D (2011) Magmatic and metamorphic imprints in 2.9 Ga chromitites from the Sittampundi layered complex, Tamil Nadu, India. Ore Geology Reviews 40, 90–107.CrossRefGoogle Scholar
Eckert, JO, Newton, RC and Kleppa, OJ (1991) The ΔH of reaction and recalibration of garnet-pyroxene-plagioclase-quartz geobarometers in the CMAS system by solution calorimetry. American Mineralogist 76, 148–60.Google Scholar
Ellis, DJ and Green, DH (1979) An experimental study of the effect of Ca upon garnet clinopyroxene Fe-Mg exchange equilibria. Contributions to Mineralogy and Petrology 71, 13–22. doi: 10.1007/BF00371878.CrossRefGoogle Scholar
Fareeduddin, and Banerjee, D.M. (2020) Aravalli Craton and its mobile belts: an update. Episodes 43, 88–108. doi: 10.18814/epiiugs/2020/020005.CrossRefGoogle Scholar
Fu, J, Liu, S, Cawood, PA, Wang, M, Hu, F, Sun, G, Gao, L and Hu, Y (2017) Neoarchean magmatic arc in the Western Liaoning Province, northern North China Craton: geochemical and isotopic constraints from sanukitoids and associated granitoids. Lithos 322, 296–311. doi: 10.1016/j.lithos.2018.10.024.CrossRefGoogle Scholar
Gamal El Dien, H, Doucet, LC, Murphy, JB and Li, ZX (2020) Geochemical evidence for a widespread mantle re-enrichment 3.2 billion years ago: implications for global-scale plate tectonics. Scientific Reports 10, 9461.CrossRefGoogle ScholarPubMed
Ganguly, J, Cheng, W and Tirone, M (1996) Thermodynamics of aluminosilicate garnet solid solution: new experimental data, an optimized model, and thermometric applications. Contributions to Mineralogy and Petrology 126, 137–51.CrossRefGoogle Scholar
Ganguly, P and Chatterjee, A (2020) Geological evolution of the northern and northwestern Eastern Ghats Belt, India from metamorphic, structural and geochronological records: an appraisal. Journal of Mineralogical and Petrological Sciences 115, 88–101.CrossRefGoogle Scholar
George, PM, Sajeev, K, Santosh, M and Zhai, M (2019) Granulite-grade garnet pyroxenite from the Kolli-massif, southern India: implications for Archean crustal evolution. Lithos 342–343, 499–512. doi: 10.1016/j.lithos.2019.05.040.CrossRefGoogle Scholar
Ghosh, B and Konar, R (2011) Chromites from meta-anorthosites, Sittampundi layered igneous complex, Tamil Nadu, southern India. Journal of Asian Earth Science 42, 1394–402. doi: 10.1016/j.jseaes.2011.07.024.CrossRefGoogle Scholar
Ghosh, B and Konar, R (2012) Textural developments in chromite deforming under eclogite-facies conditions from the Neoarchaean Sittampundi anorthosite complex, southern India. Geological Journal 47, 253–62. doi: 10.1002/gj.1316.CrossRefGoogle Scholar
Ghosh, JG, de Wit, MJ and Zartman, RE (2004) Age and tectonic evolution of Neoproterozoic ductile shear zones in the Southern Granulite Terrain of India, with implications for Gondwana studies. Tectonics 23, TC3006. doi: 10.1029/2002TC001444.CrossRefGoogle Scholar
Gopalakrishnan, M, Venkata Rao, V and Viswanathan, TV (1990) Role of palaeosutures in the evolution of southern Indian granulite terrain. In Group Discussion on Suture Zones; Young and Old (abstract), pp. 55–60. Dehadrun: Wadia Institute of Himalayan Geology.Google Scholar
Graham, CM and Powell, R (1984) A garnet–amphibole geothermometer: calibration, testing, and application to the Pelona Schist, Southern California. Journal of Metamorphic Geology 2, 13–31.CrossRefGoogle Scholar
Griffin, WL, Jensen, BB and Misra, SN (1971) Anomalously elongated rutile in eclogite-facies pyroxene and garnet. Norsk Geologisk Tidsskrift 51, 177–85.Google Scholar
Guo, B, Liu, S, Santosh, M and Wang, W (2017) Neoarchean arc magmatism and crustal growth in the north-eastern North China Craton: evidence from granitoid gneisses in the Southern Jilin Province. Precambrian Research 303, 30–53. doi: 10.1016/j.precamres.2016.12.009.CrossRefGoogle Scholar
Han, YS, Santosh, M, Ganguly, S and Li, SS (2019) Evolution of a Mesoarchean suprasubduction zone mantle wedge in the Dharwar Craton, southern India: evidence from petrology, geochemistry, zircon U–Pb geochronology, and Lu–Hf isotopes. Geological Journal 54, 2935–56. doi: 10.1002/gj.3440.CrossRefGoogle Scholar
Harris, NBW, Santosh, M and Taylor, PN (1994) Crustal evolution in south India: constraints from Nd isotopes. Journal of Geology 102, 139–50.CrossRefGoogle Scholar
He, HL, Wang, YQ, George, PM, Sajeev, K, Guo, JH, Lai, CK and Zhai, MG (2021) Formation of ∼2.5 Ga Sittampundi anorthosite complex in southern India: implications to lower crustal stabilization of the Dharwar Craton. Precambrian Research 354, 106012. doi: 10.1016/j.precamres.2020.106012.CrossRefGoogle Scholar
Holland, TJ and Powell, R (2011) An improved and extended internally consistent thermodynamic dataset for phases of petrological interest, involving a new equation of state for solids. Journal of Metamorphic Geology 29, 333–83. doi: 10.1111/j.1525-1314.2010.00923.x.CrossRefGoogle Scholar
Huang, B, Kusky, T, Johnson, T, Wilde, SA, Wang, L, Polat, A and Fu, D (2020) Paired metamorphism in the Neoarchean: a record of accretionary-to-collisional orogenesis in the North China Craton. Earth and Planetary Science Letters 543, 116355.CrossRefGoogle Scholar
Irvine, TN and Baragar, WRA (1971) A guide to the chemical classification of the common volcanic rocks. Canadian Journal of Earth Sciences 8, 523–48.CrossRefGoogle Scholar
Jan, MQ and Howie, RA (1981) The mineralogy and geochemistry of the metamorphosed basic and ultrabasic rocks of the Jijal Complex, Kohistan, NW Pakistan. Journal of Petrology 22, 85–126. doi: 10.1093/petrology/22.1.85.CrossRefGoogle Scholar
Jennings, ES and Holland, TJB (2015) A simple thermodynamic model for melting of peridotite in the system NCFMASOCr. Journal of Petrology 56, 869–92. doi: 10.1093/petrology/egv020.CrossRefGoogle Scholar
Karmakar, S, Mukherjee, S, Sanyal, S and Sengupta, P (2017) Origin of peraluminous minerals (corundum, spinel, and sapphirine) in a highly calcic anorthosite from the Sittampundi Layered Complex, Tamil Nadu, India. Contributions to Mineralogy and Petrology 172, 1–23. doi: 10.1007/s00410-017-1383-8.CrossRefGoogle Scholar
Keller, CB and Schoene, B (2018) Plate tectonics and continental basaltic geochemistry throughout Earth history. Earth and Planetary Science Letters 481, 290–304.CrossRefGoogle Scholar
Kohn, MJ and Spear, FS (1990) Two new barometers for garnet amphibolites with applications to eastern Vermont. American Mineralogist 75, 89–96.Google Scholar
Kröner, A, Santosh, M and Wong, J (2012) Zircon ages and Hf isotopic systematics reveal vestiges of Mesoproterozoic to Archaean crust within the late Neoproterozoic–Cambrian high-grade terrain of southernmost India. Gondwana Research 21, 876–86.CrossRefGoogle Scholar
Kusky, T, Wang, L, Robinson, PT, Huang, Y, Wirth, R, Ning, W, Zhong, Y and Polat, A (2021) Ultra-high pressure inclusion in Archean ophiolitic podiform chromitite in mélange block suggests deep subduction on early Earth. Precambrian Research 362, 106318.CrossRefGoogle Scholar
Laurent, O, Martin, H, Moyen, JF and Doucelance, R (2014) The diversity and evolution of late-Archean granitoids: evidence for the onset of “modern-style” plate tectonics between 3.0 and 2.5 Ga. Lithos 205, 208–35. doi: 10.1016/j.lithos.2014.06.012.CrossRefGoogle Scholar
Leake, BE, Wooley, AR and Arps, CES (1997) Nomenclature of amphiboles. Report of the subcommittee on amphiboles of the International Mineralogical Association Commission on New Minerals and Mineral Names. European Journal of Mineralogy 9, 623–51.CrossRefGoogle Scholar
Li, SS, Santosh, M and Palin, RM (2018) Metamorphism during the Archean-Paleoproterozoic transition associated with microblock amalgamation in the Dharwar Craton, India. Journal of Petrology 59, 2435–62. doi: 10.1093/petrology/egy102.CrossRefGoogle Scholar
Liu, S, Santosh, M, Wang, W, Bai, X and Yang, P (2011) Zircon U–Pb chronology of the Jianping Complex: implications for the Precambrian crustal evolution history of the northern margin of North China Craton. Gondwana Research 20, 48–63. doi: 10.1016/j.gr.2011.01.003.CrossRefGoogle Scholar
Loose, D and Schenk, V (2018) 2.09 Ga old eclogites in the Eburnian-Transamazonian orogen of southern Cameroon: significance for palaeoproterozoic plate tectonics. Precambrian Research 304, 1–11. doi: 10.1016/j.precamres.2017.10.018.CrossRefGoogle Scholar
Lu, JS, Zhai, MG, Lu, LS, Wang, H, Chen, HX, Peng, T, Wu, CM and Zhao, TP (2017) Metamorphic P-T-t path retrieved from metapelites in the southeastern Taihua Metamorphic Complex, and the Paleoproterozoic tectonic evolution of the southern North China Craton. Journal of Asian Earth Science 134, 352–64.CrossRefGoogle Scholar
Ludwig, KR (2012) User’s Manual for Isoplot 3.7. Berkeley, California: Berkeley Geochronology Center, Special Publication no. 4.Google Scholar
Mahan, KH, Goncalves, P, Flowers, R, Williams, ML and Hoffman-Setka, D (2008) The role of heterogeneous strain in the development and preservation of a polymetamorphic record in high-P granulites, western Canadian Shield. Journal of Metamorphic Geology 26, 669–94.CrossRefGoogle Scholar
Meißner, B, Deters, P, Srikantappa, C and Köhler, H (2002) Geochronological evolution of the Moyar, Bhavani and Palghat shear zones of southern India: implications for East Gondwana correlations. Precambrian Research 114, 149–75.CrossRefGoogle Scholar
Melnik, A, Korolev, N, Skublov, S, Müller, D, Li, Q and Li, X (2021) Zircon in mantle eclogite xenoliths: a review. Geological Magazine 158, 1371–82. doi: 10.1017/S0016756820001387.CrossRefGoogle Scholar
Moecher, DP, Essene, EJ and Anovitz, LM (1988) Calculation and application of clinopyroxene-garnet-plagioclase-quartz geobarometers. Contributions to Mineralogy and Petrology 100, 92–106.CrossRefGoogle Scholar
Morimoto, N (1988) Nomenclature of pyroxenes. Mineralogy and Petrology 39, 55–76.CrossRefGoogle Scholar
Mukherjee, S, Dey, A, Sanyal, S and Sengupta, P (2019) Proterozoic crustal evolution of the Chotanagpur Granite Gneissic Complex, Jharkhand-Bihar-West Bengal, India: current status and future prospect. In Tectonics and Structural Geology: Indian Context (ed. Mukherjee, S), pp. 7–54. Cham: Springer International Publishing. doi: 10.1007/978-3-319-99341-6_2.CrossRefGoogle Scholar
Nelson, DR (2006) CONCH: a visual basic program for interactive processing of ion microprobe analytical data. Computers and Geosciences 32, 1479–98.CrossRefGoogle Scholar
Newton, RC, Charlu, TV and Kleppa, OJ (1980) Thermochemistry of the high structural state plagioclases. Geochimica et Cosmochimica Acta 44, 933–41.CrossRefGoogle Scholar
Noack, NM, Kleinschrodt, R, Kirchenbaur, M, Fonseca, ROC and Munker, C (2013) Lu–Hf isotope evidence for Paleoproterozoic metamorphism and deformation of Archean oceanic crust along the Dharwar Craton margin, southern India. Precambrian Research 233, 206–22.CrossRefGoogle Scholar
Nutman, AP, Bennett, VC, Friend, CRL and Yi, K (2020) Eoarchean contrasting ultra-high-pressure to low-pressure metamorphisms (<250 to >1000 °C/GPa) explained by tectonic plate convergence in deep time. Precambrian Research 344, 105770.CrossRefGoogle Scholar
O’Brien, PJ and Rötzler, J (2003) High-pressure granulites: formation, recovery of peak conditions and implications for tectonics. Journal of Metamorphic Geology 21, 3–20. doi: 10.1046/j.1525-1314.2003.00420.x.CrossRefGoogle Scholar
Paces, JB and Miller, JD (1993) Precise U-Pb ages of Duluth Complex and related mafic intrusions, northeastern Minnesota: geochronological insights to physical, petrogenetic, paleomagnetic, and tectonomagmatic processes associated with the 1.1 Ga Midcontinent Rift System. Journal of Geophysical Research – Solid Earth 98, 13997–4013.CrossRefGoogle Scholar
Pearce, JA and Norry, MJ (1979) Petrogenetic implications of Ti, Zr, Y and Nb variations in volcanic rocks. Contributions to Mineralogy and Petrology 69, 33–47.CrossRefGoogle Scholar
Perchuk, LL, Aranovich, LYa, Podlesskii, KK, Lavrant’eva, IV, Gerasimov, VY, Fed’kin, VV, Kitsul, VI, Karsakov, LP and Berdnikov, NV (1985) Precambrian granulites of the Aldan Shield, eastern Siberia, USSR. Journal of Metamorphic Geology 3, 265–310.CrossRefGoogle Scholar
Perkins, D and Chipera, SJ (1985) Garnet-orthopyroxene-plagioclase-quartz barometry: refinement and application to the English River suprovince and the Minnesota River valley. Contributions to Mineralogy and Petrology 89, 69–80.CrossRefGoogle Scholar
Peterman, EM, Reddy, SM, Saxey, DW, Snoeyenbos, DR, Rickard, WDA, Fougerouse, D and Kylander-Clark, ARC (2016) Nanogeochronology of discordant zircon measured by atom probe microscopy of Pb-enriched dislocation loops. Science Advances 2. doi: 10.1126/sciadv.1601318.CrossRefGoogle ScholarPubMed
Peucat, JJ, Jayananda, M, Chardon, D, Capdevila, R, Fanning, C and Paquette, JL (2013) The lower crust of the Dharwar Craton, Southern India: patchwork of Archean granulitic domains. Precambrian Research 227, 4–28.CrossRefGoogle Scholar
Peucat, JJ, Mahabaleswar, B and Jayananda, M (1993) Age of younger tonalitic magmatism and granulitic metamorphism in the South Indian transition zone (Krishnagiri area); comparison with older Peninsular gneisses from the Gorur–Hassan area. Journal of Metamorphic Geology 11, 879–88.CrossRefGoogle Scholar
Plavsa, D, Collins, AS, Foden, JD and Clark, C (2015) The evolution of a Gondwanan collisional orogen: a structural and geochronological appraisal from the Southern Granulite Terrane, South India. Tectonics 34, 820–57. doi: 10.1002/2014TC003706.CrossRefGoogle Scholar
Plavsa, D, Collins, AS, Foden, JF, Kropinski, L, Santosh, M, Chetty, TRK and Clark, C (2012) Delineating crustal domains in Peninsular India: age and chemistry of orthopyroxene-bearing felsic gneisses in the Madurai Block. Precambrian Research 198–199, 77–93.CrossRefGoogle Scholar
Polat, A, Appel, PWU and Fryer, B (2011a) An overview of the geochemistry of Eoarchean to Mesoarchean ultramafic to mafic volcanic rocks, SW Greenland: implications for mantle depletion and petrogenetic processes at subduction zones in the early Earth. Gondwana Research 20, 255–83.CrossRefGoogle Scholar
Polat, A, Appel, PWU, Fryer, B, Windley, B, Frei, R, Samson, IM and Huang, H (2009) Trace element systematics of the Neoarchean Fiskenæsset anorthosite complex and associated meta-volcanic rocks, SW Greenland: evidence for a magmatic arc origin. Precambrian Research 175, 87–115.CrossRefGoogle Scholar
Polat, A, Frei, R, Appel, PWU, Dilek, Y, Fryer, B, Ordóñez-Calderón, JC and Yang, Z (2008) The origin and compositions of Mesoarchean oceanic crust: evidence from the 3075 Ma Ivisaartoq greenstone belt, SW Greenland. Lithos 100, 293–321.CrossRefGoogle Scholar
Polat, A, Frei, R, Longstaffe, FJ and Woods, R (2018) Petrogenetic and geodynamic origin of the Neoarchean Doré Lake Complex, Abitibi subprovince, Superior Province, Canada. International Journal of Earth Sciences 107, 811–43.CrossRefGoogle Scholar
Polat, A, Fryer, B, Appel, PWU, Kalvig, P, Kerrich, R, Dilek, Y and Yang, Z (2011b) Geochemistry of anorthositic differentiated sills in the Archean (∼2970 Ma) Fiskenæsset Complex, SW Greenland: implications for parental magma compositions, geodynamic setting, and secular heat flow in arcs. Lithos 123, 50–72.CrossRefGoogle Scholar
Prakash, D, Singh, PC, Tewari, S, Joshi, M, Frimmel, HE, Hokada, T and Rakotonandrasana, T (2017) Petrology, pseudosection modelling and U-Pb geochronology of silica-deficient Mg-Al granulites from the Jagtiyal section of Karimnagar granulite terrane, northeastern Dharwar Craton, India. Precambrian Research 299, 177–94.CrossRefGoogle Scholar
Raharimahefa, T and Kusky, TM (2009) Structural and remote sensing analysis of the Betsimisaraka Suture in north eastern Madagascar. Gondwana Research 15, 14–27.CrossRefGoogle Scholar
Raith, MM, Brandt, S, Sengupta, P, Berndt, J, John, T and Srikantappa, C (2016) Element mobility and behaviour of zircon during HT metasomatism of ferroan basic granulite at Ayyarmalai, South India: evidence for polyphase neoarchaean crustal growth and multiple metamorphism in the Northeastern Madurai Province. Journal of Petrology 57, 1729–74. doi: 10.1093/petrology/egw057.Google Scholar
Raith, MM, Srikantappa, C, Buhl, D and Koehler, H (1999) The Nilgiri enderbites, South India: nature and age constraints on protolith formation, high-grade metamorphism and cooling history. Precambrian Research 98, 129–50. doi: 10.1016/S0301-9268(99)00045-5.CrossRefGoogle Scholar
Ram Mohan, M, Satyanarayanan, M, Santosh, M, Sylvester, PJ, Tubrett, M and Lam, R (2013) Neoarchean suprasubduction zone arc magmatism in southern India: geochemistry, zircon U-Pb geochronology and Hf isotopes of the Sittampundi Anorthosite Complex. Gondwana Research 23, 539–57. doi: 10.1016/j.gr.2012.04.004.CrossRefGoogle Scholar
Ramakrishnan, M (1993) Tectonic evolution of the granulite terrains of southern India. Memoirs of the Geological Society of India 25, 35–44.Google Scholar
Rao, YJ, Chetty, TRK, Janardhan, AS and Gopalan, K (1996) Sm-Nd and Rb-Sr ages and PT history of the Archean Sittampundi and Bhavani layered meta-anorthosite complexes in Cauvery shear zone, South India: evidence for Neoproterozoic reworking of Archean crust. Contributions to Mineralogy and Petrology 125, 237–50.CrossRefGoogle Scholar
Ratheesh-Kumar, RT, Windley, BF, Xiao, WJ, Jia, XL, Mohanty, DP and Zeba-Nezrin, FK (2020) Early growth of the Indian lithosphere: implications from the assembly of the Dharwar Craton and adjacent granulite blocks, southern India. Precambrian Research 336, 105491. doi: 10.1016/j.precamres.2019.105491.CrossRefGoogle Scholar
Richter, FM (1988) A major change in the thermal state of the earth at the Archean-Proterozoic boundary: consequences for the nature and preservation of continental lithosphere. Journal of Petrology Special Volume 1, 39–52. doi: 10.1093/petrology/Special_Volume.1.39.CrossRefGoogle Scholar
Saha, S, Das, K, Hidaka, H, Kimura, K, Chakraborty, PP and Hayasaka, Y (2016) Detrital zircon geochronology (U-Pb SHRIMP and LA-ICPMS) from the Ampani Basin, Central India: implication for provenance and Mesoproterozoic tectonics at East Indian cratonic margin. Precambrian Research 281, 363–83.CrossRefGoogle Scholar
Saitoh, Y, Tsunogae, T, Santosh, M, Chetty, TRK and Horie, K (2011) Neoarchean high-pressure metamorphism from the northern margin of the Palghat-Cauvery Suture Zone, southern India: petrology and zircon SHRIMP geochronology. Journal of Asian Earth Science 42, 268–85. doi: 10.1016/j.jseaes.2010.11.015.CrossRefGoogle Scholar
Sajeev, K, Windley, BF, Connolly, JAD and Kon, Y (2009) Retrogressed eclogite (20 kbar, 1020 °C) from the Neoproterozoic Palghat-Cauvery suture zone, southern India. Precambrian Research 171, 23–36. doi: 10.1016/j.precamres.2009.03.001.CrossRefGoogle Scholar
Samuel, VO, Sajeev, K, Hokada, T, Horie, K and Itaya, T (2015) Neoarchean arc magmatism followed by high-temperature, high-pressure metamorphism in the Nilgiri Block, southern India. Tectonophysics 662, 109–24. doi: 10.1016/j.tecto.2015.06.035.CrossRefGoogle Scholar
Samuel, VO, Santosh, M, Liu, S, Wang, W and Sajeev, K (2014) Neoarchean continental growth through arc magmatism in the Nilgiri Block, southern India. Precambrian Research 245, 146–73. doi: 10.1016/j.precamres.2014.02.002.CrossRefGoogle Scholar
Santosh, M (2020) The southern granulite terrane: a synopsis. Episodes 43, 110–23. doi: 10.18814/EPIIUGS/2020/020006.CrossRefGoogle Scholar
Santosh, M, Maruyama, S and Yamamoto, S (2009) The making and breaking of supercontinents: some speculations based on superplumes, super downwelling and the role of tectosphere. Gondwana Research 15, 324–41. doi: 10.1016/j.gr.2008.11.004.CrossRefGoogle Scholar
Santosh, M, Shaji, E, Tsunogae, T, Ram Mohan, M, Satyanarayanan, M and Horie, K (2013) Suprasubduction zone ophiolite from Agali Hill: petrology, zircon SHRIMP U-Pb geochronology, geochemistry and implications for Neoarchean plate tectonics in southern India. Precambrian Research 231, 301–24. doi: 10.1016/j.precamres.2013.04.003.CrossRefGoogle Scholar
Santosh, M, Xiao, WJ, Tsunogae, T, Chetty, TRK and Yellappa, T (2012) The Neoproterozoic subduction complex in southern India: SIMS zircon U-Pb ages and implications for Gondwana assembly. Precambrian Research 192–195, 190–208. doi: 10.1016/j.precamres.2011.10.025.CrossRefGoogle Scholar
Santosh, M, Yang, Q-Y, Shaji, E, Ram Mohan, M, Tsunogae, T and Satyanarayanan, M (2016) Oldest rocks from Peninsular India: evidence for Hadean to Neoarchean crustal evolution. Gondwana Research 29, 105–35.CrossRefGoogle Scholar
Santosh, M, Yang, QY, Shaji, E, Tsunogae, T, Mohan, MR and Satyanarayanan, M (2015) An exotic Mesoarchean microcontinent: the Coorg Block, southern India. Gondwana Research 27, 165–95.CrossRefGoogle Scholar
Santosh, M, Yokoyama, K and Acharyya, SK (2004) Geochronology and tectonic evolution of Karimnagar and Bhopalpatnam Granulite Belts, Central India. Gondwana Research 7, 501–18. doi: 10.1016/S1342-937X(05)70801-7.CrossRefGoogle Scholar
Sato, K, Santosh, M, Tsunogae, T, Chetty, TRK and Hirata, T (2011) Subduction-accretion-collision history along the Gondwana suture in southern India: a laser ablation ICP-MS study of zircon chronology. Journal of Asian Earth Science 40, 162–71. doi: 10.1016/j.jseaes.2010.08.008.CrossRefGoogle Scholar
Schneider, CA, Rasband, WS and Eliceiri, KW (2012) NIH Image to ImageJ: 25 years of image analysis. Nature Methods 9, 671–5. doi: 10.1038/nmeth.2089.CrossRefGoogle ScholarPubMed
Sengupta, P, Raith, MM, Kooijman, E, Talukdar, M, Chowdhury, P, Sanyal, S, Mezger, K and Mukhopadhyay, D (2015) Provenance, timing of sedimentation and metamorphism of metasedimentary rock suites from the Southern Granulite Terrane, India. Geological Society of London Memoirs 43, 297–308. doi: 10.1144/M43.20.CrossRefGoogle Scholar
Shervais, JW (1982) Ti-V plots and the petrogenesis of modern and ophiolitic lavas. Earth and Planetary Science Letters 59, 101–18.CrossRefGoogle Scholar
Sotiriou, P and Polat, A (2020) Comparisons between Tethyan anorthosite-bearing ophiolites and Archean anorthosite-bearing layered intrusions: implications for Archean geodynamic processes. Tectonics 39, e2020TC006096. doi: 10.1029/2020TC006096.CrossRefGoogle Scholar
Stüwe, K (1997) Effective bulk composition changes due to cooling: a model predicting complexities in retrograde reaction textures. Contributions to Mineralogy and Petrology 129, 43–52.CrossRefGoogle Scholar
Subramaniam, AP (1956) Mineralogy and petrology of the Sittampundi Complex, Salem district, Madras State, India. Geological Society of America Bulletin 67, 317–90.CrossRefGoogle Scholar
Sun, SS and McDonough, WF (1989) Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes. Geological Society, London, Special Publications 42, 313–45.CrossRefGoogle Scholar
Talukdar, M, Mukhopadhyay, D, Sanyal, S and Sengupta, P (2019) Early Palaeoproterozoic structural reconstitution of a suite of rocks from the Mahadevi Layered Complex, Tamil Nadu, India. Geological Journal 55, 3615–42. doi: 10.1002/gj.3618.CrossRefGoogle Scholar
Talukdar, M, Sanyal, S and Sengupta, P (2017) Metasomatic alteration of chromite from parts of the late Archaean Sittampundi Layered Magmatic Complex (SLC), Tamil Nadu, India. Ore Geology Review 90, 148–65. doi: 10.1016/j.oregeorev.2017.05.021.CrossRefGoogle Scholar
Tappe, S, Smart, KA, Pearson, DG, Steenfelt, A and Simonetti, A (2011) Craton formation in Late Archean subduction zones revealed by first Greenland eclogites. Geology 39, 1103–6. doi: 10.1130/G32348.1.CrossRefGoogle Scholar
Teale, W, Collins, AS, Foden, J, Payne, JL, Plavsa, D, Chetty, TRK, Santosh, M and Fanning, M (2011) Cryogenian (∼830 Ma) mafic magmatism and metamorphism in the northern Madurai Block, southern India: a magmatic link between Sri Lanka and Madagascar? Journal of Asian Earth Science 42, 223–33. doi: 10.1016/j.jseaes.2011.04.006.CrossRefGoogle Scholar
van Hunen, J and Moyen, JF (2012) Archean subduction: fact or fiction? Annual Review of Earth and Planetary Sciences 40, 195–219. doi: 10.1146/annurev-earth-042711-105255.CrossRefGoogle Scholar
Wang, CQ and Cui, WY (1994) Granulites from the Dengchang–Houshan area, northern Hebei Province: geochemistry and metamorphism. In Geological Evolution of the Granulite Terrain in the Northern Part of the North China Craton (eds Qian, XL and Wang, RM), pp. 166–75. Beijing: Seismological Press.Google Scholar
Wei, CJ, Zhang, CG, Zhang, AL, Wu, TH and Li, JH (2001) Metamorphic P-T conditions and geological significance of high-pressure granulite from the Jianping Complex, western Liaoning province. Acta Petrologica Sinica 17, 269–82.Google Scholar
White, RW, Powell, R, Holland, TJ, Johnson, TE and Green, EC (2014) New mineral activity–composition relations for thermodynamic calculations in metapelitic systems. Journal of Metamorphic Geology 32, 261–86. doi: 10.1111/jmg.12071.CrossRefGoogle Scholar
Whitney, DL and Evans, BW (2010) Abbreviations for names of rock-forming minerals. American Mineralogist 95, 185–7. doi: 10.2138/am.2010.3371.CrossRefGoogle Scholar
Wilson, AF (1976) Aluminium in coexisting pyroxenes as a sensitive indicator of changes in metamorphic grade within the Mafic Granulite Terrane of the Fraser Range, Western Australia. Contributions to Mineralogy and Petrology 56, 255–77. doi: 10.1007/BF00466825.CrossRefGoogle Scholar
Windley, BF, Bishop, FC and Smith, JV (1981) Metamorphosed layered igneous complexes in Archean granulite-gneiss belts. Annual Review of Earth and Planetary Science 9, 175–98.CrossRefGoogle Scholar
Windley, BF, Kusky, T and Polat, A (2021) Onset of plate tectonics by the Eoarchean. Precambrian Research 352, 105980. doi: 10.1016/j.precamres.2020.105980.CrossRefGoogle Scholar
Yellappa, T, Santosh, M, Chetty, TRK, Kwon, S, Park, C, Nagesh, P, Mohanty, DP and Venkatasivappa, V (2012) A Neoarchean dismembered ophiolite complex from southern India: geochemical and geochronological constraints on its suprasubduction origin. Gondwana Research 21, 246–65.CrossRefGoogle Scholar
Yellappa, T, Santosh, M and Manju, S (2019) The mafic–ultramafic complex of Salem, southern India: an analogue for Neoproterozoic Alaskan-type complex. Geological Journal 54, 3017–40. doi: 10.1002/gj.3460.Google Scholar
Yoder, HS and Tilley, CE (1962) Origin of basalt magmas: an experimental study of natural and synthetic rock systems. Journal of Petrology 3, 342–532. doi: 10.1093/petrology/3.3.342.CrossRefGoogle Scholar
Chatterjee et al. supplementary material
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