Petrography and Mineralogy of Oxbow Lake Sediments in the Ganga Alluvial Plain, India: A Case Study with Implications for Provenance and Tectonic Setting
Published: 2024-06-14
Page: 99-119
Issue: 2024 - Volume 7 [Issue 2]
Gufran Ali *
Department of Geology, Aligarh Muslim University Aligarh, U.P, India.
*Author to whom correspondence should be addressed.
Abstract
Detailed petrographic, heavy mineral, petrofacies, and XRD investigations were conducted on nineteen sediment sample from an oxbow lake in the Ganga plain. The grains are angular to sub-rounded in shape, with some sub-rounded quartz grains. The dominant constituents of the framework grains are primarily quartz, followed by rock fragments, feldspar, mica, and heavy minerals. The majority of the quartz grains are monocrystalline, exhibiting undulatory extinctions, while the remaining are polycrystalline, displaying both distinct and suture intercrystallite boundaries. The feldspar category comprises both fresh and altered varieties, including plagioclase and microcline. Additionally, biotite, as well as large flakes of muscovite and mica, have been observed. The rock fragments include various types such as quartzite, schist, gneiss, phyllite, chert, sandstone, limestone, and siltstone. The heavy minerals encompass a range of minerals such as tourmaline, garnet, opaque minerals, zircon, andalusite, kyanite, sillimanite, staurolite, actinolite/tremolite, hornblende, biotite, rutile, muscovite, chlorite and apatite. Petrographic investigations reveal that the sediments of the ox-bow lake are sublitharenites. Heavy mineral analyses confirm the possibility of mixed provenance for the ox-bow lake sediments. The ox-bow lake petrofacies indicate their derivation from cratonic interiors, recycled orogenic, and quartzose recycled provenances, under semi-humid to humid climatic conditions. The abundance of clay minerals supports the interpretations derived from petrofacies plots regarding the provenance and tectonic setting of the oxbow lake sediments. Based on the analysis of lighter and heavy minerals, it is concluded that the sediments of the oxbow lake originated from a variety of low-grade to high-grade metamorphic rocks, as well as acid and basic igneous rocks. This case study provides comprehensive insights into the sedimentological characteristics, provenance, and tectonic setting of oxbow lake sediments in the Ganga alluvial plain, contributing to the broader understanding of sedimentary processes and geological history in this region.
Keywords: Petrography, XRD, provenance, ox-bow lake, ganga plain
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References
Dickinson WR. Provenance and sediment dispersal in relation to paleotectonics and paleogeography of sedimentary basins; In: New Perspectives in Basin Analysis (Eds.) Kleinspehn KL, Paola C. 1988 (Berlin: Springer-Verlag);3–25.
Dickinson WR, Beard LS, Brakenridge GR, Erjavec JL, Ferguson RC, Inman KF, Knepp RA, Lindberg FA, Ryberg PT. Provenance of North American Phanerozoic sandstones in relation to tectonic setting. Geological Society of American Bulletin. 1983;94:222- 235.
Krynine PD. Differential sedimentation and its products during one complete geosynclinal cycle, in primer congress panamericano De Ingeniera de Minas Geology Medidlingen. 1942;20:142- 147.
Potter PE. Modern sands of South America: Composition, provenance and global significance. Geologische Rundschau. 1994;83:212-232.
Ghosh SK, Kumar R. Petrography of Neogene Siwalik sandstone of the Himalayan foreland basin, Garhwal Himalaya: Implications for source-area tectonics and climate. Geological Society of India. 2000;55(1):1–15.
Jalal P, Ghosh SK. Provenance of the Late Neogene Siwalik sandstone, Kumaun Himalayan Foreland Basin: Constraints from the metamorphic rank and index of detrital rock fragments. Journal of Earth System Science. 2012;121:781–792. Available:https://doi.org/ 10.1007/s12040-012-0189-3.
Javed A, Khan KF, Quasim MA. Petrography of the Bajocian sandstone of Joyan member, Jaisalmer basin, western Rajasthan: Implications for provenance and basin evolution. Journal of the Geological Society of India. 2023;99(1):73–87. Available:https:// doi.org/10.1007/s12594-023-2269-1.
Khan SHAISTA, Quasim MA, Ahmad AHM, Alam MM. Petrofacies and Tectono provenance of the sandstones of Jara Dome, Kachchh Gujarat. Journal of the Indian Association of Sedimentologists. 2017;34:17.
Patra A, Singh BP, Srivastava VK. Provenance of the late Paleocene sandstones of the Jaisalmer Basin, Western India. Journal of the Geological Society of India. 2014;83:657–664. Available:https:// doi.org/10.1007/s12594-014-0096-0
Gogoi M, Sarmah RK, Goswami TK, Mahanta BN, Laishram R, Saikia H, Oza B. Petrography, clay mineralogy and geochemistry of Lower Gondwana sandstones of Western Arunachal Pradesh Himalayas, India. Journal of Sedimentary Environments. 2021;6:561–583.
Available:https://doi.org/10.1007/ s43217-021-00070-7
Garzanti E, Andò S. Heavy minerals for junior woodchucks. Minerals. 2019;9(3): 148.
Mange MA, Wright DT. High-resolution heavy mineral analysis (HRHMA): A brief summary. Developments in Sedimentology. 2007;58:433-436.
Morton AC. Heavy minerals in provenance studies. In: Zuffa, G.G. (Ed.) Provenance of Arenites, D. Reidel, Dordrecht. 1985; 249-277.
a. Garrison EG, Hale JC, Cameron CS, Smith E. The archeology, sedimentology and paleontology of Gray's Reef National Marine Sanctuary and nearby hard bottom reefs along the mid continental shelf of the Georgia Bight. Journal of Archaeological Science: Reports. 2016;5: 240-62.
Dickinson WR, Suczek CA. Plate-tectonics and sandstones composition. The American Association of Petroleum Geologists Bulletin. 1979;63:2164- 2182.
Valloni R, Mezzardi G. Compositional suites of terrigeneous deep-sea sands of the present continental margins. Sedimentology. 1984;31:353-364.
Dickinson WR. Interpreting relations from detrital modes of sandstone. In: G.G. Zuffa (Eds.), Provenance of Arenites. Reidel, Dordrecht-Boston Lancaster. 1985;333-361.
Valloni R. Reading provenance from modern marine sands. In: G.G. Zuffa (Ed), Provenance of Arenites. Reidel, Dordrecht. 1985;148:309-332.
Composition. In Provenance of Arenites Dordrecht: Springer Netherlands. 19-45.
Velbel MA. Geochemical mass balances and weathering rates in forested watersheds of the southern Blue Ridge. American Journal of Science. 1985; 285 (10):904-930.
Suttner LJ. Sedimentary petrographic provinces: An evaluation. SEPM Special Publication. 1974;21:75-84.
Mack GH. Exceptions to the relationship between plate tectonics and sandstone composition. Journal of Sedimentary Research. 1984;54(1):212-220.
Basu A. Influence of climate and relief on compositions of sands released at source areas. Provenance of Arenites. 1985;1-18.
Suttner LJ, Dutta PK. Alluvial sandstones composition and paleoclimate, I, framework mineralogy. Journal of Sedimentary Petrology. 1986;56:329-345.
Grantham JH, Velbel MA. The influence of climate and topography on rock-fragments abundance in modem fluvial sands of the southern Blue Ridge Mountains, North Carolina. Jour. Sed. Petrology. 1988;58: 219-227.
Girty GH. A note on the composition of plutoniclastic sand produced in different climatic belts, (short notes). Jour. Sed. Petrology. 1991;61:428 - 433.
Akhtar K, Ahmad AHM. Single-cycle cratonic quartzarenites produced by tropical weathering: The Nimar Sandstone (Lower Cretaceous), Narmada basin, India. Sed. Geology. 1991;71:23-32.
Mackei W. The sands and sandstones of eastern Moray, Edinburgh. Geol. Soc. Trans. 1896;7:148-172.
Krynine PD. Petrology and genesis of the Third Bradford sand, Bull. Pennysylvania Stat Coll. Min. Ind. Expt. Sta. 1940;29:134.
Krynine PD. Microscopic morphology of quartz types. An. 2"'' Cong. Panames. Ing. Minas. Geology. 1946;3:35-49.
Folk RL. Petrology of Sedimentary Rocks. Hemphills, Austen. Texas. 1980;182P.
Blatt H, Christie JM. Undulatory extinction in quartz of igneous and metamorphic rocks and its significance in provenance studies of sedimentary rocks. Jour. Sed. Petrology. 1963;38:1326 -1339.
Fuji K. Petrography of the Cretaceous sandstones of Hokkaido, Japan. Kyushu Univ. Fac. Sci. Mem. Ser. D. 1958;6:129-152.
Pettijohn FJ, Potter PE, Siever R, Pettijohn FJ, Potter PE, Siever R. Petrography of common sands and sandstones. Sand and Sandstone. 1987;139-213.
Martens JH. Persistence of feldspar in beach sand. American Mineralogist: Journal of Earth and Planetary Materials. 1931;16(11):526-531.
Russell RD. Effects of transportation on sedimentary particles: Part 1. Transportation; 1939.
Krynine PD. The megascopic study and field classification of sedimentary rocks. The Journal of Geology. 1948;56(2):130-165.
River sands. Journal of Sedimentary Research. 32(4):793-800.
Pittman ED. Use of zoned plagioclase as an indicator of Provenance. Jour. Sed. Petrology. 1963;33:380-386.
Rim Saite J. Optical heterogeneity of feldspars observed in diverse Canadian rocks. Schweiz. Mem. Pet. Mitt. 1967;47: 61-76.
Field ME, Pilkey OH. Feldspar in Atlantic continental margin sands off the SE United states. Bull. Geol. Soc. America. 1969;80: 2097-2102.
Pettijohn FJ. Sedimentary Rocks, Harper and Brothers, New York. 1975;628.
Pettijohn FJ. Sedimentary Rocks (2"'' ed.), New York, Harper and Bros. 1957;718.
Milner HB. Sedimentary Petrography Partll. George Allen and Unwin Ltd.London. 1962;715.
Boswell PGH. Mineralogy of sedimentary rocks. London Thos. Murby and Co. 1933; 393.
Krumbein WC, Pettijohn FJ. Manual of Sedimentary Petrography. Applaton Century, Inc. New York. 1938;549.
Feo-Codecido G. Heavy mineral techniques and their apphcation to Venezuela stratigraphy. Am. Assoc. Petrol. Geol. Bu Uettin. 1956;40:984-1000.
Derry LA, France-Lanord C. Neogene Himalayan weathering history and river87Sr86Sr: Impact on the marine SR record. Earth and Planetary Science Letters. 1996;142(1-2):59-74.
Robinson DM, DeCelles PG, Patchett PJ, Garzione CN. The kinematic evolution of the Nepalese Himalaya interpreted from ND isotopes. Earth and Planetary Science Letters. 2001;192(4):507-521.
Najman Y, Carter A, Oliver G, Garzanti E. Provenance of Eocene foreland basin sediments, Nepal: Constraints to the timing and diachroneity of early Himalayan orogenesis. Geology. 2005;33(4):309- 312.
Singh SK, France-Lanord C. Tracing the distribution of erosion in the Brahmaputra watershed from isotopic compositions of stream sediments. Earth and Planetary Science Letters. 2002;202(3-4):645-662.
Ramesh R, Ramanathan AL, Ramesh S, Purvaja R, Subramanian V. Distribution of rare earth elements and heavy metals in the surficial sediments of the Himalayan River system. Geochemical Journal. 2000; 34(4):295-319.
Tripathy GR, Singh SK, Ramaswamy V. Major and trace element geochemistry of Bay of Bengal sediments: Implications to provenances and their controlling factors. Palaeogeography, Palaeoclimatology, Palaeoecology. 2014;397:20-30.
Singh LB, Ghosh DK. Geomorphology and neotectonic features of Indo Gangetic plain. In: Dikshit KR, Kala VS, Kaul MN. (Eds.), India: Geomorphological Diversity. Rawat Publicatios, Jaipur. 1994;270 – 286.
Singh IB. Late Quaternary history of the Ganga Plain; J. Geol. Soc. India. 2004;64: 431–454.
Srivastava P, Singh IB, Sharma M, Singhvi AK. Luminescence chronometry and Late Quaternary geomorphic history of the Ganga Plain, India. Palaeogeography, Palaeoclimatology, Palaeoecology. 2003; 197(1-2):15-41.
Dickinson WR. Tectonics and sedimentation. SEPM Society for Sedimentary Geology; 1974.
Sieber L, Armbuster JG, Quittmeyer RC. Seismicity and continental Subduction in the Himalayan arc. In: Zagros, Hindukush, Himalaya Geodynamic evolution, (Eds. Gupta HK, Delany FM), Am. Geophys. U., Washington, Geodynamic Series 3. 1981; 215- 242.
Molnar P, Tapponnier P. Cenozoic Tectonics of Asia: Effects of a Continental Collision: Features of recent continental tectonics in Asia can be interpreted as results of the India-Eurasia collision. Science. 1975;189(4201):419-426.
Ni J, Barazangi M. Seismotectonics of the Himalayan collision zone: Geometry of the under thrusting Indian plate beneath the Himalaya. Journal of Geophysical Research: Solid Earth. 1984;89(B2):1147-1163.
Molnar P. Structures and tectoncs of the Himalaya: Constrains and implications of geophysical data. Am. Rev. Earth Planet. Science. 1984;12:489- 518.
Singh IB. Late quaternary sedimentation of Ganga plain foreland basin, preoc. symp. NW Himalaya and foredeep, feb. l995. Geol. Surv. India, Spl. Pub. 1996;21 (2):161- 172.
Burbank DW, Beck RA, Mulder T, Yin A, Harrison TM. The Himalayan foreland basin. World and Regional Geology. 1996; 149-190.
DeCelles PG, Gehrels GE, Quade J, Ojha TP. Eocene‐early Miocene foreland basin development and the history of Himalayan thrusting, western and central Nepal. Tectonics. 1998;17(5):741-765.
Frence – Lanord C, Derry L, Michard A. Evolution of Himalaya since Miocne time: Isotopic and Sedimentological evidence from the Bengal fan. In: Trelor PJ, Searl MP. (eds.) Himalayan Tectonics. Geological Society, Special Publication. 1983;74:603-621.
Covey M. The evolution of foreland basins to steady state: Evidence from the western Taiwan foreland basin. Foreland Basins. 1986;77-90.
Burbank DW. Causes of recent Himalayan uplift deduced from deposited patterns in the Ganga basin, Nature. 1992;357:680-683.
Valdiya KS. The two intracrustal boundary thrusts of the Himalaya. Tectonophysics. 1980;66(4):323-348.
Krynine PD. Petrology and genesis of the Third Bradford sand, Bull. Pennysylvania Stat Coll. Min. Ind. Expt. Sta. 1940;29:134.
Fuchtbauer H. Sediments and sedimentary rocks: Part H, John Wiley and Sons, New ork. 1974;464.
Rittenhouse C. Transportation and deposition of heavy minerals. Bull. Geol. Soc. America. 1943;45:1725- 1780.
Milner HB. Sedimentary Petrography Part’ll. George Allen and Unwin Ltd. London. 1962;715.
Cox R, Lowe DR. Quantification of the effects of secondary matrix on the analysis of sandstone composition, and a petrographic-chemical technique for retrieving original framework grain modes of altered sandstones. Journal of Sedimentary Research. 1996;66(3):548-558.
Triebold S, Von Eynatten H, Luvizotto GL, Zack T. Deducing source rock lithology from detrital rutile geochemistry: An example from the Erzgebirge, Germany. Chemical Geology. 2007;244(3-4):421-436.
Meinhold G. Rutile and its applications in earth sciences. Earth-Science Reviews. 2010;102(1-2):1-28.
Triebold S, Von Eynatten H, Zack T. A recipe for the use of rutile in sedimentary provenance analysis. Sedimentary Geology. 2012;282:268-275.
Morton AC. Influences of provenance and diagenesis on detrital garnet suites in the Forties sandstone, Paleocene, central North Sea. Journal of Sedimentary Petrology. 1987;57:1027–1032.
Mange MA, Morton AC. Geochemistry of heavy minerals. Developments in Sedimentology. 2007;58:345-391.
Krippner A, Meinhold G, Morton AC, Von Eynatten H. Evaluation of garnet discrimination diagrams using geochemical data of garnets derived from various host rocks. Sedimentary Geology. 2014;306:36-52.
Stutenbecker L, Berger A, Schlunegger F. The potential of detrital garnet as a provenance proxy in the Central Swiss Alps. Sedimentary Geology. 2017;351:11-20.
Blatt H, Middleton GV, Murray RC. Origin of Sedimentary Rocks (2nd ed.): Englewood Cliffs, NJ, Prentice-Hall. 1980; 782.
Friedman GM, Johnson KG. Excise in sedimentology, John Wiley and Sons, New York. 1982;65-99.
Weltje GJ, Meijer XD, De Boer PL. Stratigraphic inversion of siliciclastic basin fills: A note on the distinction between supply signals resulting from tectonic and climatic forcing. Basin Research. 1998; 10 (1):129-153.
Graham SA, Ingersoll RV, Dickinson WR. Common provenance for lithic grains in Carboniferous sandstones from Ouachita Mountains and Black Warrior Basin. Journal of Sedimentary Research. 1976;46 (3):620-632.
Ingersoll RV, Suczek CA. Petrology and provenance of Neogene sand from Nicobar and Bengal Fans, DSDP sites 211 and 218. Jour. Sed. Petrology. 1979;49:1217- 1218.
Potter PE. Provenance of Mudstones. Mud and Mudstones. 2005;157-174.