Facies and Sedimentary Structures of the Kerur Formation, Badami Group, South India: Implications for Depositional environment

Authors

  • Venkatraman S Hegde SDM College of Engineering and Technology, Dhavalagiri, Dharwad, Karnataka 580002, India
  • Girish Havannavar 1SDM College of Engineering and Technology, Dhavalagiri, Dharwad, Karnataka 580002, India
  • Pramod T Hanamgond GSS College of Arts and Science, Belagavi, Karnataka 590006, India
  • G Shalini Global Academy of Technology, Bengaluru, Karnataka 560098, India
  • Asim Ranjan Pratihari SDM College of Engineering and Technology, Dhavalagiri, Dharwad, Karnataka 580002, India
  • Shivani Hulaji SDM College of Engineering and Technology, Dhavalagiri, Dharwad, Karnataka 580002, India

DOI:

https://doi.org/10.48165/

Keywords:

Meso-Neoproterozoic, Kerur Formation, Badami Group, Depositional environment, Facies analysis

Abstract

Facies architecture and sedimentary structures, followed by petrographic characteristics of the rocks of  the Kerur Formation of the Badami Group of Kaladgi-Badami basin exposed in the Deshnur area near  Belgaum, in South India is discussed in the present paper to understand their depositional  environment. The Kerur Formation at Deshnur comprises of conglomerate, gritty sandstone- quartz  arenite and shale. In the type area at Badami, it comprises of Kendur conglomerate, 90m thick  sequence of arenite called “the temple arenite and the Halageri shale. In the western part, at Deshnur,  near Belgaum, Kerur Formation show rhythmic variation in conglomerate and gritty sandstone  followed by medium to fine grained arenite and intercalated thin shale beds suggesting fluctuating fluvial, beach facies and shallow water depositional condition. Features of fluvial sedimentation such  as pebble beds; shallow water sedimentary features such as symmetrical ripple marks, cross bedding;  beach facies like dune lamination and Aeolian dunes; and shallow marine facies such as intercalation  of shale with sandy facies are observed. Features such as pebbles size, rounding, along with current bedding structures within the gritty layers between the pebble beds suggest fluvial discharge to an  open sea. The thicker, gentler landward-cross strata, thinner, steeper seaward cross-strata in the  herringbone cross stratification in the overlying arenite indicate the tidal modulation during their deposition. In thin section, the grit show well rounded while the quartz arenite show moderately  rounded to well rounded, medium grained, texturally and compositionally matured characters  suggesting sorting by winnowing action of waves, implying coastal environment of deposition. The  facies Architecture, sedimentary structure like tidalites indicative of interaction of tides and current  (including changes in their speed and direction) suggest tidal modulation of depositional  environment. Well rounded, moderately assorted, vein quartz rich pebbles in alternate sandy- pebbly  layers along with arkosic nature of the grits indicate periodic flashy floods dominated the surface  hydrodynamics of transport during the early phase of sedimentation.  

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References

Allen, J.R.L. (1984). Sedimentary Structures: Their Character and Physical Basis. Elsevier, Amsterdam, 663 p.

Balesh Kumar, B., Das Sharma, S., Dayal, A. M. & Kale, V. S. (1998). Occurrence of Tiny Digitate Stromatolite Yargatti Formation, Bagalkot Group, Kaladgi Basin, Karnataka, India. Current Science, 75, 360-365.

Blatt, H., Middleton, G. & Murray, R., (1980). Origin of Sedimentary rocks, Prentice- Hall, New Jersey, 634p.

Bose, P.K. & Chakraborty, P.P. (1994). Marine to fluvial transition: Proterozoic Upper Rewa Sandstone, Maihar, India. Sedimentary Geology, 89, 285–302.

Bose, P.K., Eriksson, P.G., Sarkar, S., Wright, D.T., Samanta, P., Mukhopadhyay, S., Mandal, S., Banerjee, S. & Altermann, W. (2012). Sedimentation patterns during the Precambrian: a unique record? Journal of marine and Petroleum Geology, 33, 34–68.

Bose, P.K., Mazumder, R. & Sarkar, S. (1997). Tidal sand-waves and related storm deposits in the transgressive Protoproterozoic Chaibasa Formation, India. Precambrian Research, 84, 63–81.

Bridge, J.S. & Best, J.L. (1988). Flow, sediment transport and bedform dynamics over the transition from dunes to upper stage plane beds—implications for the formation of planar laminae.

Sedimentology, 35, 753–763.

Chakraborty, P.P., Sarkar, A., Das, K. & Das, P. (2009). Alluvial fan to storm dominated shelf transition in the

Mesoproterozoic Singhora Group, Chattisgarh Super-group, Central India. Precambrian Research, 170, 88–106.

Collinson, J.D., (1996). Alluvial sediments. In: Reading, H.G. (Ed.), Sedimentary Environments: Process, Facies and Stratigraphy. Third ed. Blackwell Science, Oxford, pp. 37–82.

De Boer, P.L., Oost, A.P. & Visser, M.J. (1989). The diurnal inequality of the tideas a parameter for recognising tidal influences. Journal of Sedimentary Petrology, 59,912–921.

Devli, M. & Mahender, K. (2018). Paleocurrent, Deformation and Geochemical studies of Lower part of the Bagalkot Group of Kaladgi Basin at Ramthal and Salgundi: Implications on Sedimentation History Jour. Indian Association of Sedimentologists, 35, (1), 77- 88; ISSN 0970-3268

Dickinson, W.R., Beard, S.L., Brakenridge, G.R., Erjavec, J.L., Ferguson, R.C., Inman, K.F., Knepp, R.A., Lindberg, F.A. & Ryberg, P.T. (1983). Provenance of North American Phanerozoic sandstones in relation to tectonic setting: Geological

Society of America Bulletin, 94, 222–235. 13. Eriksson, K.A.,(1979). Marginal marine depositional processes from the Archaean Moodies Group, Barberton Mountain Land, South Africa: evidence and significance. Precambrian Research, 8, 153– 182.

Eriksson, K.A. & Simpson, E.L. (1998). Controls on spatial and temporal distribution of Precambrian eolianites. Sedimentary Geology, 120, 275–294.

Eriksson, K.A. & Simpson, E.L. (2004). Precambrian tidalites: recognition and significance. In: Eriksson, P.G., Altermann, W., Nelson, D., Mueller, W., Cateneau, O.,Strand, K. (Eds.), Tempos and Events in Precambrian Time. Developments in Precambrian Geology 12. Elsevier, Amsterdam, pp. 631–642.

Eriksson, K.A. & Simpson, E.L. (2012). Precambrian tidal facies. In: Davis, R.A., Dalrymple, R.W.C. (Eds.), Principles of Tidal Sedimentology. Springer, pp. 397–420.

Eriksson, P.G., Banerjee, S. & Catuneanu, O. (2013). Secular changes in sedimentation systems and sequence stratigraphy. Gondwana Research, 24, 468–

Eriksson, P.G., Condie, K.C., Tirsgaard, H., Muller, W.U. Altermann, W. & Catuneanu, O., (1998). Precambrian clastic sedimentation systems.Sedimentary Geology, 120, 5–53.

Fedo, C.M. & Cooper, J.D., (1990). Braided fluvial to marine transition; the basal Lower Cambrian Wood Canyon Formation, southern Marble Mountains, Mojave Desert, California. Journal of Sedimentary Petrology, 60, 220–234.

George, T.S. (1999) Sedimentology of Kaladgi basin. In: Field workshop on integrated evolution of the Kaladgi and Bhima basins. Geological Society of India, pp.13-17.

Grotzinger, J.P. & Arvidson, R.E. (2005). Stratigraphy and sedimentology of a dry to wet eolian depositional system, Burns formation, Meridiani Planum, Mars. Earth Planetary Science Letters, 240, 11–72.

Harris, C.W. & Eriksson, K.A. (1990). Allogenic controls on the evolution of storm to tidal shelf sequences in the Early Proterozoic Uncompahgre Group, southwest Colorado, USA. Sedimentology,

, 189–213.

Hegde, V.S., Krishnaprasad, P.A., Shalini, G. & Rajawat, A.S. (2021). Granulometric dynamics of the coastal sediments of the Central West coast of India: Insight into morpho-tectonic influences on the beach processes. Catena.

https://doi.org/10.1016/j.catena.2021.105 363

Hegde, V.S., Shalini, G., Nayak, S.R., Rajawat, A.S., & Suryanarayana, A. (2009). Low scale morphodynamic process in the vicinity of a tropical estuary at Honnavar, central west coast of India. Journal of Coastal Research, 25, 305-314.

Jayaprakash, AV, Sundaram V., Hans, S.K. & Mishra R.N. (1987). Geology of the Kaladgi-Badami Basin.Purana Basins of Peninsular India (Middle to Late Proterozoic). Mem. Geol. Soc. India, 6, 201– 226.

Johnson, H.D. & Baldwin, C.T. (1996). Shallow clastic seas. In: Reading, H.G. (Ed.), Sedimentary Environments: Processes, Facies and Stratigraphy. Third ed. Blackwell, pp. 232–280.

Kocurek, G., (1991). Interpretation of ancient eolian sand dunes. Annu. Rev. Earth Planet. Sci., 19, 43–75.

Kocurek, G. (1996). Desert aeolian systems. In: Reading, H.G. (Ed.), Sedimentary Environments: Process, Facies and Stratigraphy. Third ed. Blackwell Science, Oxford, England, pp. 125– 153.

Kulkarni, K. G and Borkar, V. D. (1997). On Occurrence of Cochlichnus in the Proterozoic Rocks of Kaladgi Basin. Gondwana Geol. Magz. 12, 55-59.

Long, D.G.F. (1978). Proterozoic stream deposits: some problems of recognition and interpretation of ancient sandy fluvial systems. In: Miall, A.D. (Ed.), Fluvial Sedimentology, Canadian Society of Petroleum Geology Memoir, 5, pp. 313–341.

Longhitano, S.G., Mellere, D., Steel, R.J. & Ainsworth, R.B. (2012). Tidal depositional, systems in the rock record: a review and new insights. Sedimentary Geology, 279, 2– 22.

Martin, D.M., Powell, C.M. & George, A.D. (2000). Stratigraphic architecture and evolution of the early Paleoproterozoic McGrath Trough, Western Australia. Precambrian Research, 99, 33–64.

Mazumder, R. (2000). Turbulence particle interactions and their implications for sediment transport and bed-form mechanics under unidirectional current: some recent developments. Earth Science Review, 50, 113–124.

Mazumder, R. (2004). Implications of lunar orbital periodicities from Chaibasa tidal rhythmite of late Paleoproterozoic age. Geology, 32, 841–844.

Mazumder, R. (2005). Proterozoic sedimentation and volcanism in the Singhbhum crustal province, India and their implications. Sedimentary Geology, 176,167–193.

Mazumder, R., Van Kranendonka, M.J. & Altermann, W. (2015). A marine to fluvial transition in the Paleoproterozoic Koolbye Formation, Turee Creek Group, Western Australia. Precambrian Research, 258, 161– 170.

McCormick, D.S. & Grotzinger, J.P. (1993). Distinction of Marine from Alluvial faciesin the Paleoproterozoic (1.9 Ga) Burnside Formation, Kilohigok basin, N.W.T., Canada. Journal of Sedimentary Petrology, 63, 398–419.

Miall, A.D. (1988). Facies architecture in clastic sedimentary basins. In: Kleinspehn, K., Paola, C. (Eds.), New Perspective in Basin Analysis. Springer, Berlin/Heidelberg/New York, pp. 67–81.

Mitchum, R.M., Vail, P.R. & Thompson, S. (1977a). Seismic stratigraphy and global changes of sea level, Part 2: the depositional sequence as a basic unit for stratigraphic analysis. In: Seismic Stratigraphy – Applications to Hydrocarbon Exploration (Ed. C.E. Payton), pp. 53–62.

Mukherjee, M. K., Das, S. & Modak, K., (2016). Basement-Cover Structural Relationships In: The Kaladgi Basin, Southwestern India: Indications Towards A Mesoproterozoic Gravity Gliding o f The Cover Along A Detached Unconformity. Precambrian Research, 281, 495-520.

Padmakumari, V. M., Sambasiva, Rao., V. V.& Srinivasan, R. (1998). Model Nd and Rb-Sr Ages of Shales of the Bagalkot Group, Kaladgi Supergroup, Karnataka. Nat. Symp. Late Quart. Geol and Sea Level Changes, Cochin University. Kochi Abst;70.

Ramachandran,A., Madhavaraju, J., Ramasamy, S., Lee,Y., Rao, S., Chawngthu, D.L. &Velmurgan, K., (2016). Geochemistry of Proterozoic clastic rocks of the Kerur Formation of Kaladgi-Badami Basin, North Karnataka, South India: implications for paleoweathering and provenance. Turkish Journal of Earth Science,.,doi:10.3906/yer-1503-4.

Reineck, H.E. & Singh, I.B., (1986). Depositional Sedimentary Environments; With Reference to Terrigenous Clastics. Springer, Berlin

Sathyanarayan,S., (1994). The Younger Proterozoic Badami Group, Northern Karnataka; In: ‘Geo Karnataka’, MGD Centenary volume, pp. 227–233.

Serebryakov, S.N., (1976). Biotic and biotic factors controlling the morphology of Riphean Stromatolites. In: M.R. Walter (Ed.) Stromatolites, Elsevier. Amsterdam, pp. 321-326.

Sharma M., Nair S., Patil S., Shukla M. and Kale V.S. (1998). Occurrence of tiny digitate stromatolite [Yelma Digitata Grey, 1984], Yargatti Formation, Bagalkot Group, Kaladgi Basin, Karnataka, India; Curr. Sci. 75(4), 360–365.

Singh, I. B. (1980). Precambrian sedimentary sequences in India: Their peculiarities and comparison with modern sediments Precambrian Research, 12, 411- 436.

Tirsgaard, H. (1993). The architecture of Precambrian high energy tidal channel deposits: an example from the Lyell Land Group (Eleonore Bay Supergroup), northeast Greenland. Sedimentary Geology, 88, 137–152.

Verlekar, P. A., & Kotha, M. (2020). Provenance, tectonics and palaeo environment of Mesoproterozoic Saundatti Quartzite Member of Kaladgi Basin, India: A petrographic view. Journal

of the Indian Association of Sedimentologists, 37(2), 91–102.

https://doi.org/10.51710/jias.v37i2.101

Vishwanathaiah, M.N. (1977) Lithostratigraphy of the Kaladgi and Badami Groups, Karnataka. Indian Mineralogist, 18, 122-132.

Wabo, H., De Kock, M., Beukes, N., & Hegde, V. (2020). Palaeomagnetism of the uppermost carbonate units of the Purana basins in southern India: New demagnetization results from the Kaladgi and Bhima basins, Karnataka. Geological Magazine, 1-10.

doi.org/10.1017/S0016756820001181.

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Published

2021-12-15

Issue

Vol. 40 No. 2 (2021): Bulletin of Pure and Applied Sciences Geology (Jul-Dec) 2021

Section

Articles

How to Cite

Hegde, V.S., Havannavar, G., Hanamgond, P.T., Shalini, G., Pratihari, A.R., & Hulaji, S. (2021). Facies and Sedimentary Structures of the Kerur Formation, Badami Group, South India: Implications for Depositional environment . Bulletin of Pure and Applied Sciences-Geology , 40(2), 227–243. https://doi.org/10.48165/
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