Abstract
The succession of lithofacies of a part of the Barren Measures Formation of the Talchir Gondwana basin has been studied by statistical techniques. The lithologies have been grouped under five facies states viz coarse-, medium-, and fine-grained sandstones, shale and coal for statistical analyses. Markov chain analysis indicates the arrangement of Barren Measures lithofacies in the form of fining upward cycles. A complete cycle consists of conglomerate or coarse-grained sandstone at the base sequentially succeeded by medium-and fine-grained sandstones, shales and coal at the top. The entropy analysis puts the Barren Measures cycles into A-4 type cyclicity, which consists of different proportions of lower, upper and side truncated cycles of lithologic states. Regression analysis indicates a sympathetic relationship between total thickness of strata (net subsidence) and number of cycles and an antipathic relationship between average thickness and number of sedimentary cycles. The cyclic sedimentation of the Barren Measures Formation was controlled by autocyclic process which occurred due to the lateral migration of streams triggered by intrabasinal differential subsidence. In many instances, the clastic sediments from the laterally migrating rivers interrupted the cyclic sedimentation resulting in thinner cycles in areas where the number of cycles are more. Principal component and multivariate regression analyses suggest that the net subsidence of the basin is mostly controlled by the thickness of sandstones, shale beds and coal stringers.
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References
Allen, J.R.L. (1965a) Fining upward cycles in alluvial successions. Geol. Jour., v.4, pp.229–246.
Allen, J.R.L. (1965b) A review of the origin and characteristics of recent alluvial sediments. Sedimentology, v.5, pp.89–191.
Belt, E.S., Sakimoto, S.E.H. and Rockwell, B.W. (1992) A drainage diversion hypothesis for the origin of widespread coal beds in the williston basin: Examples from Palaeocene strata, eastern Montana. In: M.A. Sholes (Ed.), Coal geology of Montana, Mon. Bureau of Mines and Geology Spec Publ., v.102, pp.21–60.
Billingsley, P. (1961) Statistical methods in chains, Arm. Math. Statist., v.32, pp.12–40.
Cant, J.C. and Walker, R.G. (1978) Fluvial processes and facies sequences in sandy braided South Saskatchewan river, Canada. Sedimentology, v.25, pp.625–468.
Casshyap, S.M. (1970) Sedimentary cycles and environment of deposition of the Barakar coal measures of Lower Gondwana, India. Jour. Sed. Petrol., v.40, pp.1302–1317.
Casshyap, S.M. (1975) Cyclic characteristics of coal-bearing sediments in the Bochumer Formation (westphal A 2) Ruhrgebiet, Germany. Sedimentology, v.22, pp.237–255.
Das, R. and Pandya, K.L. (1995) Lithofacies and environment of deposition of a part of Damuda Group, Talchir basin, Orissa. Vistas in Geological Research, Spec. Publ. Geology Utkal University, Bhubaneswar, v.1, pp.152–159.
Davis, J.C. (2002) Statistics and Data Analysis in Geology. John Wiley and Sons, 639p.
Duff, P. Mc. L.D. (1967) Cyclic sedimentation in the permian coal measures of New South Wales. Jour. Geol. Soc. Australia, v. 14, pp. 293–307.
Duff, P. Mc. L, Hallam, D. and Walton, E.K. (1967) Cyclic sedimentation. Development in Sedimentology No.10, Elsevier, 280p.
Harbaugh, J.W. and Bonham-Carter, G. (1970) Computer simulation in Geology. Wiley Interscience, New York, 575p.
Hattori, I. (1976) Entropy in Markov chain and discrimination of cyclic pattern in lithologic successions. Math. Geol., v.8, pp. 477–497.
Hota, R.N. and Maejima, W. (2004) Comparative study of cyclicity of lithofacies in Lower Gondwana formations of Talchir basin, Orissa, India: A statistical analysis of subsurface logs. Gondwana Res., v.7 (No.2), pp.353–362.
Hota, R.N. and Pandya, K.L. (2002) Quantitative relationship between net subsidence and coal cycles in Barakar Formation, Talchir coalfield, Orissa. Jour. Geol. Soc. India, v.60, pp.203–211.
Hota, R.N., Pandya, K.L. and Maejima, W. (2003) Cyclic sedimentation and facies organization of the coal bearing Barakar Formation, Talchir Gondwana basin, Orissa, India: a statistical analysis of subsurface logs. Jour. Geoscience, Osaka City Univ., Osaka, v.46, pp.1–11.
Hota, R. N., Maejima, W. and Mishra, B (2007) River metamorphosis during Damuda sedimentation: a case study from Talchir Gondwana basin, Orissa. Jour. Geol. Soc. India, v.69, pp.1351–1360.
Johnson, K.R. and Cook, A.C. (1973) Cyclic characteristics of sediments in the Moon Island Beach Subgroup, New Castle coal measures, New South Wales. Math. Geol., v.5, pp.91–110.
Kumar, R. (1990) Lithofacies association and quantitative analysis of the Upper Siwalik Subgroup in a part of Punjab Subhimalays. Jour. Indian Earth Sci., v.17, pp.180–193.
Miall, A. D. (1973) Markov Chain analysis applied to an alluvial plain succession. Sedimentology, v.20, pp.347–364.
Miall, A. D. (1977) A review of the braided-river depositional environment, Earth-Science Rev., v.13, pp.1–62.
Nichols, G. (1999) Sedimentology and Stratigraphy. Blackwell Science Ltd., 355p.
Pandya, K.L. (2006) Gondwanas. In: N.K. Mahalik, H.K. Sahoo, R.N. Hota, B.P. Mishra, J.K. Nanda, and A.B. Panigrahi (Eds.), Geology and mineral resources of Orissa, Society of Geoscientists and Allied Technologists, Bhubaneswar, pp.91–103.
Pettijohn, F.J. (1984) Sedimentary rocks. CBS Publishers and Distributers, New Delhi, 628p.
Prothero, D.R. and Schwab, F. (1996) Sedimentary Geology. W.H. Freeman and Co., New York, 573p.
Raja Rao, C.S. (1982) Coal resources of Tamilnadu, Andhra Pradesh, Orissa and Maharastra. Bull. Geol. Surv. India, No.45, pt.II, pp.41–52.
Read, W.A. and Dean, J.M. (1967) A quantitative study of a sequence of coal bearing cycles in the Namurian of Central Scotland. Sedimentology, v.9, pp.137–156.
Read, W.A. and Dean, J.M. (1972) Principal component analysis of lithologic variables from some Namurian (E2) paralic sediments in Central Scotland. Bull. Geol. Surv. Great Britain, v.40, pp.83–99
Read, W.A. and Dean, J.M. (1976) Cycles of subsidence: their relationship in different sedimentary and tectonic environments in the Scottish Carboriferous. Sedimentology, v.23, pp.107–120.
Read, W.A. and Dean, J.M. (1982) Quantitative relationships between numbers of fluvial cycles, bulk lithological composition and net subsidence in a Scottish Namurian basin. Sedimentology, v.29, pp.181–200.
Sengupta, S. (2007) Introduction to Sedimentology. CBS Publishers and Distributors, New Delhi, 314p.
Strahler, A. N. (1963) The earth sciences. Harper and Row Publishers, New York, 681p.
Shukla, U.K., Khan, Z.A. and Singh, I.B. (1996) Markov chain analysis of the shallow marine Bhuj sandstone of Early Cretaceous age, Kachchh basin, India. Jour. Geol. Soc. India, v.48, pp.567–578.
Tewari, R.C. (1995) Braided-fluvial depositional model of Late Triassic Gondwana (Mahadeva) rocks of the Son valley, Central India: Tectonic and Paleogeographic implications Jour. Geol. Soc. India, v.45, pp.65–73.
Tewari, R.C. (2008) Net subsidence and evolution of coal swamps in Early Permian coal measures of eastern India Gondwana basins using principal component analysis, Jour Geosciences, Osaka City University, Japan, v.51, pp.27–34.
Udden, J.A. (1912) Geology and mineral resources of Peoria Quadrangle, Illinois. U.S. Geol. Surv. Bull. No.506, 103p.
Weller J.M. (1930) Cyclical sedimentation of the Permsylvanian period and its significance. Jour. Geol., v.38, pp.97–135.
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Hota, R.N., Das, B.K. Cyclic sedimentation of the Barren Measures Formation (Damuda Group), Talchir Gondwana basin: Statistical appraisal from borehole logs. J Geol Soc India 75, 549–559 (2010). https://doi.org/10.1007/s12594-010-0044-6
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DOI: https://doi.org/10.1007/s12594-010-0044-6