Log in

Successive stages of interaction between felsic and mafic magma in the Bundelkhand craton, India: A petrographic investigation

  • Published:
Journal of Earth System Science Aims and scope Submit manuscript

Abstract

A complex magma mingling/interaction zone in the Bundelkhand craton, Central India, was formed when several pulses of mafic magma interacted with the still-crystallising felsic magma. Coeval emplacements of mafic−felsic magmas (marked by the cuspate−lobate boundary, crystal transfer, and hybrid rocks) produce various styles of interactions (besides the formation of the mafic magmatic enclaves). These are included in the mafic patches, hybrid enclaves, tabular sheet/dykes in the felsic rocks; granitoid back-veins and enclaves in the mafic rocks. Each interacting features exhibit distinct texture of minerals is documented. A model of coeval emplacements of mafic−felsic magmas is presented by the four successive stages of interaction. During stage I, a mixed boundary layer between the felsic and mafic phases was formed facilitating strong mechanical exchange. Mafic enclaves in the felsic phase were formed in stage II. During stage III, back-veining of the felsic melt into the mafic phase took place. Stage IV or the late stage of mingling is manifested by the formation of amoeboid titanites.

Research highlights

A complex MMZ is present in the Bundelkhand craton. The MMZ involves four stages of the interaction of the mafic−felsic magmas. Each stage exhibits a distinct textural characteristic of minerals.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Subscribe and save

Springer+ Basic
EUR 32.99 /Month
  • Get 10 units per month
  • Download Article/Chapter or Ebook
  • 1 Unit = 1 Article or 1 Chapter
  • Cancel anytime
Subscribe now

Buy Now

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Figure 1
Figure 2
Figure 3
Figure 4
Figure 5
Figure 6
Figure 7
Figure 8
Figure 9

Similar content being viewed by others

References

  • Årebäck H, Andersson U B and Petersson J 2008 Petrological evidence for crustal melting unmixing and undercooling in an alkali-calcic high-level intrusion: The late Sveconorwegian Vinga intrusion SW Sweden; Min. Petrol. 93 1–46.

    Google Scholar 

  • Barbarin B 2005 Mafic magmatic enclaves and mafic rocks associated with some granitoids of the central Sierra Nevada batholiths California nature origin and relations with the hosts; Lithos. 80 155–177.

    Google Scholar 

  • Barbarin B and Didier J 1992 Genesis and evolution of mafic microgranular enclaves through various types of interaction between coexisting felsic and mafic magmas; Trans. Roy. Soc. Edinb. Earth Sci. 83 145–153.

    Google Scholar 

  • Basu A K 1986 Geology of Bundelkhand Granite massif, Central India; Record, GSI 117 61–124.

    Google Scholar 

  • Baxter S and Feely M 2002 Magma mixing and mingling textures in granitoids examples from the Galway Granite Connemara Ireland; Min. Petrol. 76 63–74.

    Google Scholar 

  • Blundy J D and Sparks R S J 1992 Petrogenesis of mafic inclusion in granitoids of the Admello Massif, Italy; J. Petrol. 33 1039–1104.

    Google Scholar 

  • Chappell B W 1996 Magma mixing and the production of compositional variation within granite suites: Evidence from granites of southeastern Australia; J. Petrol. 37 449–470.

    Google Scholar 

  • Chen B, He J and Ma X 2009a Petrogenesis of mafic enclaves from the north Taihang Yanshanian intermediate to felsic plutons: Evidence from petrological, geochemical, and zircon Hf-O isotopic data; Sci. China Ser. D: Earth Sci. 52 1331–1344.

    Google Scholar 

  • Chen B, Chen Z C and Jahn B M 2009b Origin of mafic enclaves from the Taihang Mesozoic orogen, north China craton; Lithos 110 343–358.

    Google Scholar 

  • Chen S, Niu Y L, Li J, Sun W L, Zhang Y, Hu Y and Shao F L 2016 Syn-collisional adakitic granodiorites formed by fractional crystallization: Insights from their enclosed ma_cmagmatic enclaves (MMEs) in the Qumushan pluton, North Qilian Orogen at the northern margin of the Tibetan Plateau; Lithos 248–251 455–468.

    Google Scholar 

  • Coombs M L, Eichelberger J C and Rutherford M J 2002 Experimental and textural constraints on mafic enclave formation in volcanic rocks; J. Volcanol. Geotherm. Res. 119 12.

    Google Scholar 

  • Deb T and Bhattacharyya T 2018 Interaction between felsic granitoids and mafic dykes in Bundelkhand craton: A field petrographic and crystal size distribution study; J. Earth Syst. Sci. 127 102.

    Google Scholar 

  • Domańska-Siuda J and Bagiński B 2019 Magma mingling textures in granitic rocks of the eastern part of the Strzegom-Sobótka Massif (Polish Sudetes); Acta Geol. Prol. 69 143–160.

    Google Scholar 

  • Elangovan R, Krishna K, Vishwakarma N, Hari K R and Ram Mohan M 2017 Interaction of coeval felsic and mafic magmas from the Kanker granite, Pithora region, Bastar craton, central India; J. Earth Syst. Sci. 126 92.

    Google Scholar 

  • Gogoi B, Saikia A and Ahmad M 2017 Titanite-centered ocellar texture: A petrological tool to unravel the mechanism enhancing magma mixing; Period. Min. 86 245–273.

    Google Scholar 

  • Gokarn S G, Rao C K, Selvaraj C, Gupta G and Singh B P 2013 Crustal evolution and tectonics of the Archean Bundelkhand craton Central India; J. Geol. Soc. India 82 455–460.

    Google Scholar 

  • Griffin W L, Wang X, Jackson S E, Pearson N J, O’Reilly S Y, Xu X and Zhou X 2002 Zircon chemistry and magma mixing SE China: In situ analysis of Hf isotopes Tonglu and **tan igneous complexes; Lithos 61 237–269.

    Google Scholar 

  • Hibbard M J 1991 Textural anatomy of twelve magma-mixed granitoid systems; In: Enclaves and granite petrology (eds) Didier J and Barbarin B, Elsevier, Amsterdam, pp. 431–444.

    Google Scholar 

  • Hu H, Li J W, McFarlane C R M, Luo Y and McCarron T 2017 Textures, trace element compositions, and U–Pb ages of titanite from the mangling granitoid pluton, east Qinling Orogen: Implications for magma mixing and destruction of the North China craton; Lithos 284–285 50–68.

    Google Scholar 

  • Jayananda M, Gireesh R, Sekhamo K-U and Miyazaki T 2014 Coeval felsic and mafic magmas in Neoarchean calcalkaline magmatic arcs, Dharwar craton, Southern India: Field and petrographic evidence from mafic to hybrid magmatic enclaves and synplutonic mafic dykes; J. Geol. Soc. India 84(1) 5–28.

    Google Scholar 

  • Jiang P, Yang F, Fan H R, Liu X, Cai Y C and Yang Y H 2016 Titanite-scale insights into multi-stage magma mixing in Early Cretaceous of NW Jiaodong terrain North China craton; Lithos 258 197–214.

    Google Scholar 

  • Joshi K B, Bhattacharjee J, Rai G, Halla J, Kurhilla M, Heilimo E, Ahmad T and Whitehouse M 2017 The diversification of granitoids and plate tectonic implications at the Archaean–Proterozoic boundary in the Bundelkhand Craton, Central India; In: Crust–mantle interactions and granitoid diversification: Insights from archaean cratons (eds) Halla J, Whitehouse M J, Ahmad T and Bagai Z, Geol. Soc. London, Spec. Publ. 449 123–157.

  • Kaur P, Zeh A, Chaudhri N and Eliyas N 2016 Unravelling the record of archaean crustal evolution of the Bundelkhand craton, northern India using U–Pb zircon–Monazite ages, Lu–Hf isotope systematics, and whole-rock geochemistry of granitoids; Precamb. Res. 281 384–413.

    Google Scholar 

  • Leake B E, Woolley A R, Arps C E S and Birch W D 1997 Nomenclature of amphiboles: Report of the subcommittee on amphiboles of the International Mineralogical Association Commission on New minerals and mineral names; Min. Mag. 61 295–321.

    Google Scholar 

  • Liu D L, Shi R D, Ding L, Huang Q S, Zhang X R, Yue Y H and Zhang L Y 2017 Zircon U–Pb age and Hf isotopic compositions of Mesozoic granitoids in southern Qiangtang Tibet: Implications for the subduction of the Bangong–Nujiang Tethyan Ocean; Gondwana Res. 41 157–172.

    Google Scholar 

  • Marangoanha B, Oliveira D C, Galarza M A and Marques G T 2020 Crustal anatexis and mantle-derived magmas forming Neoarchean A-type granitoids in Carajás Province, northern Brazil: Petrological evidence and tectonic control; Precamb. Res. 338 105–585.

    Google Scholar 

  • McLeod G W, Dempster T J and Faithfull J W 2011 Deciphering magma-mixing processes using zoned titanite from the Ross of Mull granite, Scotland; J. Petrol. 52 55–82.

    Google Scholar 

  • Michel L, Wenzel T and Mark G 2017 Interaction between two contrasting magmas in the Albtal pluton (Schwarzwald SW Germany): Textural and mineral–chemical evidence; Int. J. Earth Sci. 106 1505–1524.

    Google Scholar 

  • Mondal M E A, Goswami J N, Deomurari M P and Sharma K K 2002 Ion microprobe 207Pb/206Pb ages of zircon 1426 A. I. Slabunov and V. K. Singh from the Bundelkhand massif, northern India: Implication for crustal evolution of Bundelkhand–Aravalli protocontinent; Precamb. Res. 117 85–100.

    Google Scholar 

  • Nelson S T and Montana A 1992 Sieve-textured plagioclase in volcanic rocks produced by rapid decompression; Am. Min. 77 1242–1249.

    Google Scholar 

  • Perugini D, Poli G, Christofides G and Eletheriadis G 2003 Magma mixing in the Sithonia plutonic complex, Greece: Evidence from mafic microgranular enclaves; Min. Petrol. 78 173–200.

    Google Scholar 

  • Pietranik A, Koepke J and Puziewicz J 2006 Crystallization and resorption in plutonic plagioclase: Implications on the evolution of granodiorite magma (Gęsiniec granodiorite, Strzelin Crystalline Massif, SW Poland); Lithos 86 260–280.

    Google Scholar 

  • Pradhan V R, Meert J G, Pandit M K, Kamenov G and Mondal M E A 2012 Paleomagnetic and geochronological studies of the mafic dyke swarms of Bundelkhand craton, Central India: Implications for the tectonic evolution and paleogeographic reconstructions; Precamb. Res. 198–199 51–76.

    Google Scholar 

  • Ramiz M M and Mondal M E A 2017 Petrogenesis of mafic magmatic enclaves of the Bundelkhand granitoids near Orccha Central Indian shield: Evidence for rapid crystallization; In: Crust mantle interactions and granitoid diversification: Insights from archaean cratons (eds) Halla J, Whitehouse M J, Ahmad T and Bagai Z, Geol. Soc. London, Spec. Publ. 449 159.

  • Rao M J, Poornachandra Rao G V S, Widdowson M and Kelley S P 2005 Evolution of Proterozoic mafic dyke swarms of the Bundelkhand Granite Massif, central India; Curr. Sci. 88 502–506.

    Google Scholar 

  • Sahoo D, Pruseth K L, Upadhyay D, Ranjan S, Pal D C, Banerjee R and Gupta S 2017 New constraints from zircon, monazite, and uraninite dating on the commencement of sedimentation in the Cuddapah basin, India; Geol. Mag. 147 1230–1246.

    Google Scholar 

  • Sensarma S, Matin A, Paul D, Madhesiya A K and Sarkar G 2021 Evolution of a crustal-scale silicic to intermediate tectono-magmatic system: The 2600–2300 Ma Bundelkhand granitoid; Precamb. Res. 352 1105951.

    Google Scholar 

  • Slabunov A and Singh V K 2018 Bundelkhand and Dharwar craton (Indian Shield): Comparison the crustal evolution in Archean time; Archaeol. Anthropol. 3(2) 42–48.

    Google Scholar 

  • Slabunov A and Singh V K 2019 Meso-Neoarchaean crustal evolution of the Bundelkhand craton, Indian Shield: New data from greenstone belts; Int. Geol. Rev. USA, https://doi.org/10.1080/00206814.2018.1512906.

    Article  Google Scholar 

  • Slabunov A, Singh V K, Joshi K B and Li X 2017 Paleoarchean zircons from quartzite of South Bundelkhand Supracrustal Complex: Origin and implications for crustal evolution in Bundelkhand craton, Central India; Curr. Sci. 112 794–801.

    Google Scholar 

  • Sparks R S J and Marshal L A 1986 Thermal and mechanical constraints on mixing between mafic and silicic magmas; J. Volcanol. Geotherm. Res. 29 99–124.

    Google Scholar 

  • Sun J F, Yang J H, Wu F Y, Li X H, Yang Y H, **e L W and Wilde S A 2010 Magma mixing controlling the origin of the Early Cretaceous Fangshan granitic pluton North China craton: In situ U–Pb age and Sr–Nd–Hf- and O-isotope evidence; Gondwana Res. 120 421–438.

    Google Scholar 

  • Turnbull R, Weaver S, Tulloch A, Cole J, Handler M and Ireland T 2010 Field and geochemical constraints on mafic–felsic interactions, and processes in high-level arc magma chambers: An example from the Halfmoon Pluton, New Zealand; J. Petrol., https://doi.org/10.1093/petrology/egq026.

    Article  Google Scholar 

  • Ubide T, Galé C, Larrea P, Arranz E, Lago M and Tierz P 2014 The relevance of crystal transfer to magma mixing: A case study in composite dykes from the Central Pyrenees; J. Petrol. 55 1535–1559.

    Google Scholar 

  • Vernon R H 1984 Microgranitoid enclaves: Globules of hybrid magma quenched in a plutonic environments; Nature 304 438–439.

    Google Scholar 

  • Vernon R H 1990 Crystallisation and hybridism in microgranitoid enclave magmas: Microstructural evidence; J. Geophys. Res. 95 849–859.

    Google Scholar 

  • Vernon R H 1991 Interpretation of microstructures of microgranitoid enclaves; In: Enclaves and granite petrology (eds) Didier J and Barbarin B, Elsevier, Amsterdam, pp. 277–292.

    Google Scholar 

  • Vernon R H, Etheridge M A and Wall V J 1988 Shape and microstructure of microgranitoid enclaves: Indicators of magma mingling and flows; Lithos 22 1–11.

    Google Scholar 

  • Wang Q, Li X H, Jia X H, Wyman D, Tang G J, Li Z X, Ma L, Yang Y H, Jiang Z Q and Gou G N 2012 Late Early Cretaceous adakitic granitoids and associated magnesian and potassium-rich mafic enclaves and dikes in the Tunchang-Fengmu area, Hainan Province (South China): Partial melting of lower crust and mantle, and magma hybridization; Chem. Geol. 328 222–243.

    Google Scholar 

  • Wiebe R A, Smith D, Sturn M and King E M 1997 Enclaves in the Cadillac mountain granite 494 (Coastal Maine): Samples of hybrid magma from the base of the chamber; J. Petrol. 495(38) 393–426.

    Google Scholar 

  • Whitney D L and Evans B W 2010 Abbreviations for names of rock-forming minerals; Am. Min. 95 185–203.

    Google Scholar 

  • **ao X, Zhou T F, White N C, Zhang L J, Fan Y and Chen X F 2020 Multiple generations of titanites and their geochemical characteristics record the magmatic-hydrothermal processes and timing of the Dongguashan porphyry-skarn Cu–Au system, Tongling district, Eastern China; Min. Dep. 56(1), https://doi.org/10.1007/s00126-020-00962-0.

    Article  Google Scholar 

  • Yang J H, Wu F Y, Zhang Y B, Zhang Q and Wilde S A 2004 Identification Mesoproterozoic zircons in a Triassic dolerite from the Liaodong Peninsula northeast China; Chin. Sci. Bull. 49 1958–1962.

    Google Scholar 

  • Yang J H, Wu F Y, Wilde S A, **e L W, Yang Y H and Liu X M 2007 Tracing magma mixing in granite genesis: In situ U–Pb dating and Hf-isotope analysis of zircons; Contrib. Min. Petrol. 153 177–190.

    Google Scholar 

Download references

Acknowledgements

The authors acknowledge the Earth and Environmental Science Department, Indian Institute of Science Education and Research, Bhopal for providing financial and logistic support. TD acknowledges the Geological Survey of India, Kolkata for providing laboratory support. A few data are taken from the previous work of TD. The authors thank Professor Tapas Bhattacharyya for his valuable suggestions. The authors also thank the anonymous reviewers and the editor for their valuable comments that immensely helped in improving the quality of the manuscript.

Author information

Authors and Affiliations

Authors

Contributions

The study was conceived and designed by J Mallik and T Deb. The manuscript writing and fieldwork were done by T Deb. Both the authors contributed towards the data analyses, the discussion and representation of the results.

Corresponding author

Correspondence to Jyotirmoy Mallik.

Additional information

Communicated by Rajneesh Bhutani

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Deb, T., Mallik, J. Successive stages of interaction between felsic and mafic magma in the Bundelkhand craton, India: A petrographic investigation. J Earth Syst Sci 131, 48 (2022). https://doi.org/10.1007/s12040-021-01778-w

Download citation

  • Received:

  • Revised:

  • Accepted:

  • Published:

  • DOI: https://doi.org/10.1007/s12040-021-01778-w

Keywords

Navigation