Abstract
Recognition of ancient pyroclastic rocks made up of particles of explosive volcanic origin and deposited by primary volcanic processes and/or rapid sedimentation of freshly erupted, texturally unmodified particles vis-a-vis secondary volcaniclastic deposits derived by significant reworking during transport of primary volcanic particles prior to deposition, but long after volcanism (epiclastic) remains a major challenge. A volcanic conglomerate having both rhyolitic clasts and matrix within the ~2.5 Ga Bijli Rhyolite in the Dongargarh large igneous province in the Bastar craton, is earlier interpreted to be of epiclastic origin, primarily because of the presence of large rounded rhyolite clasts imparting conglomeratic appearance to the deposit, and thereby considered representing a significant time break (unconformity) between explosive Bijli volcanism and the deposit. Based on new field and petrography studies, we identified the ~125 m thick volcanic conglomerate as rapidly sedimented texturally unmodified rhyolitic breccia-conglomerate linked to coeval incipiently welded pyroclastic flow that occurred during caldera collapse related to mafic-recharge-mediated Bijli volcanism, without significant time break. We ascribed the rounding of rhyolite clasts to surface tension of hot crystallising molten magma in plastic state and partly to mechanical interactions of particles on steep slopes in such volcanic settings. This study may help clarify origin of similar deposits in deformed metamorphosed provinces elsewhere.
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References
Bryan S E, Peate I U, Peate D W, Self S, Jerram D A, Mawby M R, Marsh J S and Miller J A 2010 The largest volcanic eruptions on Earth; Earth Sci. Rev. 102 207–229, https://doi.org/10.1016/j.earscirev.2010.07.001.
Cas R A F and Wright J V 1987 Volcanic successions: Modern and ancient; Allen and Unwin, London, 528p.
Chakraborty M, Debnath S and Mahapatro S N 2021 Lithofacies analysis of volcanics and volcaniclastics of an ancient volcanic terrain with signatures of subaerial plinian volcanism: An example from Neoarchaean–Palaeoproterozoic Nandgaon group, Bastar craton, central India; J. Earth Syst. Sci. 130 145, https://doi.org/10.1007/s12040-021-01656-5.
Chakraborty T and Sensarma S 2008 Shallow marine and coastal eolian quartz arenite in the Neoarchaean–Palaeoproterozoic Karutola formation, Dongargarh volcano-sedimentary succession, central India; Precamb. Res., https://doi.org/10.1016/j.precamres.2007.07.024.
Cheng L, Trenberth K E, Fasullo J, Boyer T, Abraham J and Zhu J 2017 Improved estimates of ocean heat content from 1960 to 2015; Sci. Adv. 3(3), https://doi.org/10.1126/sciadv.1601545.
Christiansen R L 1979 Cooling units and composite sheets in relation to caldera structure; In: Ash-flow tuffs (eds) Chapin C E and Elston W E, Geol. Soc. Am. Spec. Pap. 180 29–42.
Christiansen R L 2001 Quaternary and Pliocene volcanism of the Yellowstone Plateau region of Wyoming, Idaho, and Montana: U.S. Geol. Surv. Prof. Pap. 729-G 143.
Costa F and Chakraborty S 2004 Decadal time gaps between mafic intrusion and silicic eruption obtained from chemical zoning patterns in olivine; Earth Planet. Sci. Lett. 227 517–530, https://doi.org/10.1016/j.epsl.2004.08.011.
Deshpande G G, Mahobey N K and Deshpande M S 1990 Petrography and tectonic setting of Dongargarh volcanics; Geol. Surv. India Spec. Publ. 28 260–288.
de Silva S 2008 Arc magmatism, calderas, and supervolcanoes; Geology 36(8) 671–672, https://doi.org/10.1130/focus082008.1.
Fermor L L 1934 General report for 1934; Rec. Geol. Surv. India 67(1) 88p.
Fermor L L 1935 General report for 1934; Rec. Geol. Surv. India 68(1) 91p.
Fisher R V 1966 Rocks composed of volcanic fragments and their classification; Earth Sci. Rev. 1 287–298.
Fisher R V and Smith G A 1991 Sedimentation in volcanic settings; SEPM Spec. Publ. 45 1–5.
Fiske R S 1969 Recognition and significance of pumice in marine pyroclastic rocks; GSA Bull. 80(1) 1–8, https://doi.org/10.1130/0016-7606(1969)80[1:RASOPI]2.0.CO;2.
Freundt A and Schmincke H-U 1992 Abrasion in pyroclastic flows; Geol. Rundsch. 81(2) 383–389.
Freundt A and Schmincke H-U 1995 Eruption and emplacement of a basaltic welded ignimbrite during caldera formation on Gran Canaria; Bull. Volcanol. 56 640–659, https://doi.org/10.1007/BF00301468.
Ghose N C, Chatterjee N and Windley B F 2016 Subaqueous early eruptive phase of the late Aptian Rajmahal volcanism, India: Evidence from volcaniclastic rocks, bentonite, black shales, and oolite; Geosci. Frontiers 8 809–822, https://doi.org/10.1016/j.gsf.2016.06.007.
Ghosh J G 2004 Geochronological constraints on the evolution of the Kotri linear belt and its basement; Rec. Geol. Surv. India 136(2) 24–26.
Gooday R J, Brown D J, Goodenough K M and Kerr A C 2018 A proximal record of caldera-forming eruptions: The stratigraphy, eruptive history and collapse of the Palaeogene Arran caldera, western Scotland; Bull. Volcanol. 80(70), https://doi.org/10.1007/s00445-018-1243-z.
Gottsmann J, Lavallée Y, Martí J and Aguirre-Díaz G 2009 Magma-tectonic interaction and the eruption of silicic batholiths; Earth Planet. Sci. Lett. 284(3–4) 426–434, https://doi.org/10.1016/j.epsl.2009.05.008.
Gupta A and Basu A 2000 North Singhbhum proterozoic mobile belt eastern India – A review; Geol. Surv. India Spec. Publ. 55 195–226.
Gupta A, Basu A and Singh S K 1977 Occurrence of a pyroclastic Conglomerate in Dalma Metavolcanics, Singbhum district, Bihar; Indian J. Earth Sci. 4(2) 1601–1668.
Halder M, Paul D and Sensarma S 2021 Rhyolites in continental mafic large igneous provinces: Petrology, geochemistry and petrogenesis; Geosci. Frontiers 12(1) 53–80, https://doi.org/10.1016/j.gsf.2020.06.011.
Hedberg H D (ed.) 1976 International stratigraphic guide – A guide to stratigraphic classification, terminology and procedure; John Wiley & Sons, New York, 200p.
Krishnamurthy P, Sinha D K, Rai A K, Seth D K and Singh S N 1990 Magmatic rocks of the Dongargarh supergroup, central India – Their petrological evolution and implications on metallogeny; Geol. Surv. India Spec. Publ. 28 303–319.
Manikyamba C, Santosh M, Chandan Kumar B, Rambabu S, Tang L, Saha A, Khelen A C, Ganguly S, Singh Th D and Subba Rao D V 2016 Zircon U–Pb geochronology, Lu–Hf isotope systematics, and geochemistry of bimodal volcanic rocks and associated Granitoids from Kotri belt, central India: Implications for Neoarchean–Palaeoproterozic crustal growth; Gondwana Res. 38 313–333, https://doi.org/10.1016/j.gr.2015.12.008.
Maughan L L, Christiansen E H, Best M G, Grommé C S, Deino A L and Tingey D G 2002 The oligocene lund tuff, great basin, USA: A very large volume monotonous intermediate; J. Volcanol. Geotherm. Res. 113(1–2) 129–157, https://doi.org/10.1016/S0377-0273(01)00256-6.
McPhie J, Doyle M and Allen R 1993 Volcanic textures: A guide to the interpretation of textures in Pyroclastic Rocks. Hobart Australia: CODES Key Centre, University of Tasmania, GPO Box 252C, Hobart, Tasmania 7001, 196p.
Mukhopadhyay J, Ray A, Ghosh G, Medda R A and Bandyopadhyay P P 2001 Recognition, characterization and implications of high-grade silicic ignimbrite facies from the Palaeoproterozoic Bijli rhyolites, Dongargarh supergroup, central India; Gondwana Res. 4 519–527, https://doi.org/10.1016/S1342-937X(05)70351-8.
Müller W, Chown E H and Thurston P C 2000 Processes in physical volcanology and volcaniclastic sedimentation: Modern and ancient; Precamb. Res. 101 81–85, https://doi.org/10.1016/S0301-9268(99)00095-9.
Ramachandra H M and Roy A 1998 Geology of intrusive granitoids with particular reference to Dongargarh granite and their implication on tectonic evolution of the Precambrian in central India; Indian J. Geosci. (formerly Indian Minerals) 52 15–32.
Rooney T O, Sinha A K, Deering C and Briggs C 2010 A model for the origin of rhyolites from South Mountain, Pennsylvania: Implications for rhyolites associated with large igneous provinces; Lithosphere 2(4) 211–220, https://doi.org/10.1130/L89.1.
Ross C S and Smith R L 1961 Ash-flow tuffs: Their origin geologic relations and identification; US Geol. Surv. Prof. Pap. 360 81p.
Sarkar S N 1956 Petrography of the rhyolitic conglomerates of east Bhandara, Madhya Pradesh; Sci. Cult. 23 51–53.
Sarkar S N 1957 Stratigraphy and tectonics of Dongargarh system: A new system in the Precambrian of Bhandara–Durg–Balaghat area, Bombay and Madhya Pradesh; J. Sci. Eng. Res. 1(2) 237–268.
Sarkar S N 1958 Stratigraphy and tectonics of Dongargarh system: A new system in the Precambrian of Bhandara–Durg–Balaghat area, Bombay and Madhya Pradesh; J. Sci. Eng. Res. 2(2) 145–160.
Sarkar S N 1994 Chronostratigraphy and tectonics of the Dongargarh supergroup Precambrian rocks in Bhandara–Durg region, central India; Indian J. Earth Sci. 21 19–31.
Sarkar S N, Gopalan K and Trivedi J R 1981 New data on the geochronology of the Precambrians of Bhandara–Durg, central India; Indian J. Earth. Sci. 8 131–151.
Schmid R 1981 Descriptive nomenclature and classification of pyroclastic deposits and fragments: Recommendations of the IUGS Subcommission on the systematics of igneous rocks; Geology 9 41–43.
Sensarma S 2005 The Dongargarh Group: A large Igneous Province at the Archean-Proterozoic Transition in India. AGU Chapman Conference, The Great Plume Debate: The origin and impact of LIPs and hot spots 87.
Sensarma S 2007 A bimodal LIP and the plume debate: The Palaeoproterozoic Dongargarh group, Central India; Geol. Soc. Am. Spec. Paper 430 831–839.
Sensarma S, Hoernes S and Mukhopadhyay D 2004 Relative contributions of crust and mantle to the origin of the Bijli rhyolite in a Palaeoproterozoic bimodal volcanic sequence (Dongargarh group), central India; J. Earth Syst. Sci. 113 619–648, https://doi.org/10.1007/BF02704026.
Sensarma S and Mukhopadhyay D 2003 New insight on the stratigraphy and volcanic history of the Dongargarh belt, central India; Gondwana Geol. Mag. Spec. 7 129–136.
Sensarma S and Mukhopadhyay D 2014 Stratigraphy of the ~2.5 Ga Dongargarh belt, central India: Key observations and suggested revisions; Gondwana Geol. Mag. Spec. 16 41–48.
Sensarma S and Palme H 2013 Silicate liquid immiscibility in the ~2.5 Ga Fe-rich andesite at the top of the Dongargarh large igneous province (India); Lithos 170–171 239–251, https://doi.org/10.1016/j.lithos.2013.03.004.
Sensarma S, Palme H and Mukhopadhyay D 2002 Crust-mantle interaction in the genesis of siliceous high magnesian basalts (SHMB): Evidence from the early Proterozoic Dongargarh supergroup, India; Chem. Geol. 187 21–37, https://doi.org/10.1016/S0009-2541(02)00020-7.
Sensarma S, Singh H, Rana R S, Paul D and Sahni A 2017 Nature and composition of interbedded marine basaltic pumice in the ∼52–50 Ma Vastan lignite sequence, western India: Implication for Early Eocene MORB volcanism offshore Arabian Sea; J. Earth Syst. Sci. 126(2), https://doi.org/10.1007/s12040-017-0806-2.
Sensarma S, Storey B C and Malviya V P 2018 Gondwana large igneous provinces: Distribution, diversity and significance; Geol. Soc. London, Spec. Publ. 463 1–16.
Sharkove E, Bogina M and Chistyakov A 2017 Magmatic systems of large continental igneous provinces; Geosci. Frontiers 8 621–640, https://doi.org/10.1016/j.gsf.2016.03.006.
Sharma K K 2004 The Neoproterozoic Malani magmatism of the northwestern Indian shield: Implications for crust-building processes; Proc. Indian Acad. Sci. (Earth Planet. Sci.) 113(4) 795–807.
Shellnutt J G, Bhat G M, Wang K-L, Brookfield M E, Dostal J and Jahn B-M 2012 Origin of the silicic volcanic rocks of the Early Permian Panjal traps, Kashmir, India; Chem. Geol. 334 154–170, https://doi.org/10.1016/j.chemgeo.2012.10.022.
Sohn C and Sohn Y K 2019 Distinguishing between primary and secondary volcaniclastic deposits; Sci. Rep. 9 12425, https://doi.org/10.1038/s41598-019-48933-4.
Storm S, Shane P, Schmitt A K and Lindsay J M 2011 Contrasting punctuated zircon growth in two syn-erupted rhyolite magmas from Tarawera volcano: Insights to crystal diversity in magmatic systems; Earth Planet. Sci. Lett. 301 511–520, https://doi.org/10.1016/j.epsl.2010.11.034.
Troll V R, Emeleus C H, Nicoll G R, Mattsson T, Ellam R M, Donaldson C H and Harris C 2019 A large explosive silicic eruption in the British Palaeogene igneous province; Sci. Rep., https://doi.org/10.1038/s41598-018-35855-w.
Vallinayagam G and Kumar N 2007 Volcanic vent in Nakora ring complex of Malani igneous suite, northwestern India; J. Geol. Soc. India 70(5) 881–883.
White J D L, Bryan S E, Ross P-S, Self S and Thordarson T 2009 Physical volcanology of continental large igneous provinces: Update and review. In studies in volcanology: The legacy of George Walker; IAVCEI Spec. Publ. 2 291–321, https://doi.org/10.1144/IAVCEl002.15.
Wilson C J N 2008 Supereruptions and supervolcanoes: Processes and products; Elements 4 29–34, https://doi.org/10.2113/GSELEMENTS.4.1.29.
Wright J V, Smith A L and Self S 1980 A working terminology for pyroclastic deposits; J. Volcanol. Geotherm. Res. 8 315–336, https://doi.org/10.1016/0377-0273(80)90111-0.
Acknowledgements
Authors acknowledge Prof Dhruba Mukhopadhyay (formerly of the University of Calcutta), for introducing SS to the fascinating geology of the Dongargarh province long back, Prof N V Chalapathi Rao and Prof J S Ray (the guest editors) for the invitation to contribute to this special volume in memory of late Prof Gautam Sen, an acclaimed petrologist of our time, Department of Geology, University of Lucknow for support. The paper is benefitted from the comments of two anonymous reviewers.
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First author: Fieldwork; formulation of the idea, overall technical supervision. Both authors: Participated in thin-section petrography study, interpretation, writing and preparation of the final manuscript.
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Communicated by Jyotisankar Ray
This article is part of the Topical Collection: Deccan Traps and other Flood Basalt Provinces – Recent Research Trends.
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Sensarma, S., Gaur, R. Origin of silicic breccio-conglomerate within the ~2.5 Ga LIP rhyolites, Bastar craton (India) and its volcanological and stratigraphic implications. J Earth Syst Sci 131, 105 (2022). https://doi.org/10.1007/s12040-022-01840-1
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DOI: https://doi.org/10.1007/s12040-022-01840-1