Abstract
The petrographic and geochemical composition of the Dharla River sediments has been examined to infer their sediment type, degree of weathering, provenance, and tectonic settings. Petrographically the sediments are characterized by the high quartz content (64.97 to 74.24 wt%), followed by feldspar (7.04 to 15.20 wt%), mica (5.38 to 19.92 wt%), lithic fragment (3.46 to 8.14 wt%), and heavy minerals (1.98 to 6.94 wt%). Geochemical composition shows marked enrichment of SiO2 (mean ~ 74.16%) and a strong negative correlation with the other major oxides because of quartz dilution. The Chemical index of alteration (CIA, 45.52 to 63.51); Plagioclase index of alteration (PIA, 43.13 to 66.55); W index (20.15 to 32.86) and Rb/Sr ratios (0.35 to 0.98) suggest low to moderate intensity of chemical weathering in the source area. Geochemical classifications of the studied samples show mostly litharenitic immature type of sediments also reflects high index of compositional variability (ICV, 0.96 to 1.72). The ternary diagrams of Al2O3–(CaO + Na2O)–K2O (or A–CN–K) and of mafic rocks, felsic rocks and degree of weathering of the source rocks (or MFW) and several immobile trace element ratios (e.g. light rare earth element/Light rare earth element or LREE /HREE, Eu/Eu*, LaN/LuN, La/Sc, La/Co, Th/Sc, and Th/Co) reflect the contribution of common felsic source rock, with the composition close to average rhyolite, granodiorite, and granite. Chondrite‐normalized rare earth element (REE) pattern shows high LREE enrichments and almost flat HREE pattern with a sharp negative Eu anomaly suggesting a felsic source provenance and characteristically supports the Himalayan source rocks compositions seemingly observed in both active and passive continental margins. The geochemical nature of weathering patterns manifests the Dharla somewhat of mass distributor en route the Brahmaputra to the global ocean.
Similar content being viewed by others
References
Akarish, A., & El-Gohary, A. (2011). Provenance and source area weathering derived from the geochemistry of Pre-Cenomanian sandstones, East Sinai Egypt. Journal of Applied Sciences, 11(17), 3070–3088. https://doi.org/10.3923/jas.2011.3070.3088.
Basu, A., Young, S. W., Suttner, L. J., James, W. C., & Mack, G. H. (1975). Re-evaluation of the use of undulatory extinction and polycrystallinity in detrital quartz for provenance interpretation. Journal of Sedimentary Research, 45(4), 873–882. https://doi.org/10.1306/212F6E6F-2B24-11D7-8648000102C1865D.
Bayon, G., Toucanne, S., Skonieczny, C., André, L., Bermell, S., Cheron, S., et al. (2015). Rare earth elements and neodymium isotopes in world river sediments revisited. Geochimica et Cosmochimica Acta, 170, 17–38. https://doi.org/10.1016/j.gca.2015.08.001.
Bhatia, M. R. (1983). Plate tectonics and geochemical composition of sandstones. The Journal of Geology, 91(6), 611–627. https://doi.org/10.1086/628815.
Bhatia, M. R., & Crook, K. A. W. (1986). Trace element characteristics of graywackes and tectonic setting discrimination of sedimentary basins. Contributions to Mineralogy and Petrology, 92(2), 181–193. https://doi.org/10.1007/BF00375292.
Bhuiyan, M. A. H., Rahman, M. J. J., Dampare, S. B., & Suzuki, S. (2011). Provenance, tectonics and source weathering of modern fluvial sediments of the Brahmaputra-Jamuna River, Bangladesh: Inference from geochemistry. Journal of Geochemical Exploration, 111(3), 113–137. https://doi.org/10.1016/j.gexplo.2011.06.008.
Bikramaditya Singh, R. K. (2010). Geochemistry and petrogenesis of granitoids of Lesser Himalayan crystallines, Western Arunachal Himalaya. Journal of the Geological Society of India, 75(4), 618–631. https://doi.org/10.1007/s12594-010-0055-3.
Blatt, H. (1985). Provenance studies and Mudrocks. SEPM Journal of Sedimentary Research. https://doi.org/10.1306/212F8611-2B24-11D7-8648000102C1865D.
Bose, I., & Navera, U. K. (2017). Flood maps and bank shifting of Dharla River in Bangladesh. Journal of Geoscience and Environment Protection, 5(09), 109. https://doi.org/10.4236/gep.2017.59008.
Bracciali, L., Marroni, M., Pandolfi, L., & Rocchi, S. (2007). Geochemistry and petrography of Western Tethys Cretaceous sedimentary covers (Corsica and Northern Apennines): from source areas to configuration of margins. Geological Society of America Special Papers, 420, 73. https://doi.org/10.1130/2006.2420(06).
Camuti, K. S., & McGuire, P. T. (1999). Preparation of polished thin sections from poorly consolidated regolith and sediment materials. Sedimentary Geology, 128(1–2), 171–178. https://doi.org/10.1016/S0037-0738(99)00073-1.
Caracciolo, L., Von Eynatten, H., Tolosana-Delgado, R., Critelli, S., Manetti, P., & Marchev, P. (2012). Petrological, geochemical, and statistical analysis of eocene-oligocene sandstones of the Western Thrace Basin, Greece and Bulgaria. Journal of Sedimentary Research, 82(7), 482–498. https://doi.org/10.2110/jsr.2012.31.
Carosi, R., Montomoli, C., & Iaccarino, S. (2018). 20 years of geological mapping of the metamorphic core across Central and Eastern Himalayas. Earth-Science Reviews, 177, 124–138. https://doi.org/10.1016/j.earscirev.2017.11.006.
Chakraborty, S., & Datta, K. (2013). Causes and consequences of channel changes–a spatio-temporal analysis using remote sensing and GIS—Jaldhaka-Diana River System (Lower Course), Jalpaiguri (Duars), West Bengal, India. Journal of Geography and Natural Disasters, 3(1), 1–13. https://doi.org/10.4172/2167-0587.1000107.
Chakraborty, S., & Mukhopadhyay, S. (2014). A comparative study on the nature of channel confluence dynamics in the lower Jaldhaka River system, West Bengal, India. International Journal of Geology, Earth and Environmental Sciences, 4(2), 87–97.
Chaudhuri, S., & Brookins, D. G. (1979). The RbSr systematics in acid-leached clay minerals. Chemical Geology, 24(3–4), 231–242. https://doi.org/10.1016/0009-2541(79)90125-6.
Cohen, J. (2013). Statistical power analysis for the behavioral sciences. Routledge. https://doi.org/10.4324/9780203771587.
Condie, K. C. (1993). Chemical composition and evolution of the upper continental crust: contrasting results from surface samples and shales. Chemical Geology, 104(1–4), 1–37. https://doi.org/10.1016/0009-2541(93)90140-E.
Condie, K. C., Noll, P. D., & Conway, C. M. (1992). Geochemical and detrital mode evidence for two sources of Early Proterozoic sedimentary rocks from the Tonto Basin Supergroup, central Arizona. Sedimentary Geology, 77(1–2), 51–76. https://doi.org/10.1016/0037-0738(92)90103-X.
Cox, R., Lowe, D. R., & Cullers, R. L. (1995). The influence of sediment recycling and basement composition on evolution of mudrock chemistry in the southwestern United States. Geochimica et Cosmochimica Acta, 59(14), 2919–2940. https://doi.org/10.1016/0016-7037(95)00185-9.
Crook, K. A. W. (1974). Lithogenesis and geotectonics: the significance of compositional variation in flysch arenites (graywackes). SEPM Society for Sedimentary Geology Special Publication, 19, 304–310.
Cullers, R. L. (1994). The controls on the major and trace element variation of shales, siltstones, and sandstones of Pennsylvanian-Permian age from uplifted continental blocks in Colorado to platform sediment in Kansas, USA. Geochimica et Cosmochimica Acta, 58(22), 4955–4972. https://doi.org/10.1016/0016-7037(94)90224-0.
Das, B. K., & Haake, B. G. (2003). Geochemistry of Rewalsar Lake sediment, Lesser Himalaya, India: implications for source-area weathering, provenance, and tectonic setting. Geosciences Journal, 7(4), 299–312. https://doi.org/10.1007/BF02919560.
Dasgupta, S., Ganguly, J., & Neogi, S. (2004). Inverted metamorphic sequence in the Sikkim Himalayas: crystallization history, P-T gradient, and implications. Journal of Metamorphic Geology, 22(5), 395–412. https://doi.org/10.1111/j.1525-1314.2004.00522.x.
Derakhshan-Babaei, F., Nosrati, K., Tikhomirov, D., Christl, M., Sadough, H., & Egli, M. (2020). Relating the spatial variability of chemical weathering and erosion to geological and topographical zones. Geomorphology, 363, 107235. https://doi.org/10.1016/j.geomorph.2020.107235.
Dickinson, W. R. (1985). Interpreting Provenance Relations from Detrital Modes of Sandstones. In Provenance of Arenites (pp. 333–361). Dordrecht: Springer Netherlands. https://doi.org/https://doi.org/10.1007/978-94-017-2809-6_15
Dickinson, W. R., Beard, L. S., Brakenridge, G. R., Erjavec, J. L., Ferguson, R. C., Inman, K. F., et al. (1983). Provenance of North American Phanerozoic sandstones in relation to tectonic setting. Geological Society of America Bulletin, 94(2), 222. https://doi.org/10.1130/0016-7606(1983)94%3c222:PONAPS%3e2.0.CO;2.
Dickinson, W. R., & Suczek, C. A. (1979). Plate tectonics and sandstone compositions. AAPG Bulletin, 63, 2164–2182. https://doi.org/10.1306/2F9188FB-16CE-11D7-8645000102C1865D.
Fedo, C. M., Nesbitt, H. W., & Young, G. M. (1995). Unraveling the effects of potassium metasomatism in sedimentary rocks and paleosols, with implications for paleoweathering conditions and provenance. Geology, 23(10), 921. https://doi.org/10.1130/0091-7613(1995)023%3c0921:UTEOPM%3e2.3.CO;2.
Folk, R. L. (1974). Petrology of sedimentary rocks. Austin: Hemphill Publishing Company.
Galy, A., & France-Lanord, C. (2001). Higher erosion rates in the Himalaya: geochemical constraints on riverine fluxes. Geology, 29(1), 23. https://doi.org/10.1130/0091-7613(2001)029%3c0023:HERITH%3e2.0.CO;2.
Ghosh, S., Sarkar, S., & Ghosh, P. (2012). Petrography and major element geochemistry of the Permo-Triassic sandstones, central India: Implications for provenance in an intracratonic pull-apart basin. Journal of Asian Earth Sciences, 43(1), 207–240. https://doi.org/10.1016/j.jseaes.2011.09.011.
Hayashi, K. I., Fujisawa, H., Holland, H. D., & Ohmoto, H. (1997). Geochemistry of ∼19 Ga sedimentary rocks from northeastern Labrador Canada. Geochimica et Cosmochimica Acta, 61(19), 4115–4137. https://doi.org/10.1016/S0016-7037(97)00214-7.
Herron, M. M. (1988). Geochemical classification of terrigenous sands and shales from core or log data. SEPM Journal of Sedimentary Research. https://doi.org/10.1306/212F8E77-2B24-11D7-8648000102C1865D.
Holeman, J. N. (1968). The Sediment yield of major Rivers of the World. Water Resources Research, 4(4), 737–747. https://doi.org/10.1029/WR004i004p00737.
Hossain, H. M. Z. (2020). Major, trace, and REE geochemistry of the Meghna River sediments, Bangladesh: Constraints on weathering and provenance. Geological Journal, 55(5), 3321–3343. https://doi.org/10.1002/gj.3595.
Hossain, I., Roy, K. K., Biswas, P. K., Alam, M., Moniruzzaman, M., & Deeba, F. (2014). Geochemical characteristics of Holocene sediments from Chuadanga district, Bangladesh: Implications for weathering, climate, redox conditions, provenance and tectonic setting. Chinese Journal of Geochemistry, 33(4), 336–350. https://doi.org/10.1007/s11631-014-0696-9.
Howarth, R. J. (1998). Improved estimators of uncertainty in proportions, point-counting, and pass-fail test results. American Journal of Science, 298(7), 594–607.
Ingersoll, R. V., Bullard, T. F., Ford, R. L., Grimm, J. P., Pickle, J. D., & Sares, S. W. (1984). The Effect of grain size on detrital modes: a test of the gazzi-dickinson point-counting method. SEPM Journal of Sedimentary Research, 54(1), 103–116.
Islam, R., Ghosh, S. K., Vyshnavi, S., & Sundriyal, Y. P. (2011). Petrography, geochemistry and regional significance of crystalline klippen in the Garhwal Lesser Himalaya India. Journal of Earth System Science, 120(3), 489–501. https://doi.org/10.1007/s12040-011-0086-1.
Jacobson, A. D., Blum, J. D., Chamberlain, C. P., Craw, D., & Koons, P. O. (2003). Climatic and tectonic controls on chemical weathering in the New Zealand Southern Alps. Geochimica et Cosmochimica Acta, 67(1), 29–46. https://doi.org/10.1016/S0016-7037(02)01053-0.
Jin, Z., Li, F., Cao, J., Wang, S., & Yu, J. (2006). Geochemistry of Daihai Lake sediments, Inner Mongolia, north China: implications for provenance, sedimentary sorting, and catchment weathering. Geomorphology, 80(3–4), 147–163. https://doi.org/10.1016/j.geomorph.2006.02.006.
Kohn, M. J., Paul, S. K., & Corrie, S. L. (2010). The lower Lesser Himalayan sequence: a Paleoproterozoic arc on the northern margin of the Indian plate. Geological Society of America Bulletin, 122(3–4), 323–335. https://doi.org/10.1130/B26587.1.
Kroonenberg, S. B. (1994). Effects of provenance, sorting and weathering on the geochemistry of fluvial sands from different tectonic and climatic environments. In Proceedings of the 29th international geological congress, Part A (Vol. 69, p. 81).
Kundu, A., Matin, A., & Eriksson, P. G. (2016). Petrography and geochemistry of the Middle Siwalik sandstones (tertiary) in understanding the provenance of sub-Himalayan sediments in the Lish River Valley, West Bengal India. Arabian Journal of Geosciences, 9(2), 162. https://doi.org/10.1007/s12517-015-2261-1.
Kundu, A., Matin, A., & Mukul, M. (2012). Depositional environment and provenance of Middle Siwalik sediments in Tista valley, Darjiling District, Eastern Himalaya India. Journal of Earth System Science, 121(1), 73–89. https://doi.org/10.1007/s12040-012-0154-1.
Suttner, L. J., & Dutta, P. K. (1986). Alluvial Sandstone Composition and Paleoclimate, I. Framework Mineralogy. SEPM Journal of Sedimentary Research. https://doi.org/10.1306/212F8909-2B24-11D7-8648000102C1865D.
Li, L., Ni, J., Chang, F., Yue, Y., Frolova, N., Magritsky, D., et al. (2020). Global trends in water and sediment fluxes of the world’s large rivers. Science Bulletin, 65(1), 62–69. https://doi.org/10.1016/j.scib.2019.09.012.
Long, X., Yuan, C., Sun, M., Safonova, I., Xiao, W., & Wang, Y. (2012). Geochemistry and U-Pb detrital zircon dating of Paleozoic graywackes in East Junggar, NW China: insights into subduction–accretion processes in the southern Central Asian Orogenic Belt. Gondwana Research, 21(2–3), 637–653. https://doi.org/10.1016/j.gr.2011.05.015.
López, J. M. G., Bauluz, B., Fernández-Nieto, C., & Oliete, A. Y. (2005). Factors controlling the trace-element distribution in fine-grained rocks: the Albian kaolinite-rich deposits of the Oliete Basin (NE Spain). Chemical Geology, 214(1–2), 1–19. https://doi.org/10.1016/j.chemgeo.2004.08.024.
Macdonald, E. H. (2007). Handbook of gold exploration and evaluation (1st Edition). Woodhead Publishing.
Maharana, C., Srivastava, D., & Tripathi, J. K. (2018). Geochemistry of sediments of the Peninsular rivers of the Ganga basin and its implication to weathering, sedimentary processes and provenance. Chemical Geology, 483, 1–20. https://doi.org/10.1016/j.chemgeo.2018.02.019.
Mange, M. A., & Maurer, H. (1992). Heavy minerals in colour. Berlin: Springer Science & Business Media.
Martin, J. M., & Meybeck, M. (1979). Elemental mass-balance of material carried by major world rivers. Marine Chemistry, 7(3), 173–206. https://doi.org/10.1016/0304-4203(79)90039-2.
McLennan, S. M. (1989). Rare earth elements in sedimentary rocks: influence of provenance and sedimentary processes. Reviews in Mineralogy and Geochemistry, 21(1), 169–200.
McLennan, S. M., Hemming, S., McDaniel, D. K., & Hanson, G. N. (1993). Geochemical approaches to sedimentation, provenance, and tectonics. Geological Society of America Special Papers. https://doi.org/10.1130/SPE284-p21.
McQuarrie, N., Robinson, D., Long, S., Tobgay, T., Grujic, D., Gehrels, G., & Ducea, M. (2008). Preliminary stratigraphic and structural architecture of Bhutan: implications for the along strike architecture of the Himalayan system. Earth and Planetary Science Letters, 272(1–2), 105–117. https://doi.org/10.1016/j.epsl.2008.04.030.
Miller, C., Thoni, M., Frank, W., Grasemann, B., Klotzli, U., Guntli, P., & Draganits, E. (2001). The early Palaeozoic magmatic event in the Northwest Himalaya, India: source, tectonic setting and age of emplacement. Geological Magazine, 138(3), 237–251. https://doi.org/10.1017/S0016756801005283.
Milliman, J. D., & Meade, R. H. (1983). World-wide delivery of river sediment to the oceans. The Journal of Geology, 91(1), 1–21. https://doi.org/10.2307/30060512.
Mottram, C. M., Argles, T. W., Harris, N. B. W., Parrish, R. R., Horstwood, M. S. A., Warren, C. J., & Gupta, S. (2014). Tectonic interleaving along the Main Central Thrust, Sikkim Himalaya. Journal of the Geological Society, 171(2), 255–268. https://doi.org/10.1144/jgs2013-064.
Mukul, M. (2010). First-order kinematics of wedge-scale active Himalayan deformation: insights from Darjiling–Sikkim–Tibet (DaSiT) wedge. Journal of Asian Earth Sciences, 39(6), 645–657. https://doi.org/10.1016/j.jseaes.2010.04.029.
Nakayama, K., & Nakamura, T. (2005). X-ray fluorescence analysis of rare earth elements in rocks using low dilution glass beads. Analytical Sciences, 21(7), 815–822. https://doi.org/10.2116/analsci.21.815.
Nesbitt, H. W., & Young, G. M. (1982). Early Proterozoic climates and plate motions inferred from major element chemistry of lutites. Nature, 299(5885), 715–717. https://doi.org/10.1038/299715a0.
Nesbitt, H. W., & Young, G. (1984). Prediction of some weathering trends of plutonic and volcanic rocks based on thermodynamic and kinetic considerations. Geochimica et Cosmochimica Acta, 48(7), 1523–1534. https://doi.org/10.1016/0016-7037(84)90408-3.
Ni, J. F. (1989). Active tectonics of the Himalaya. Journal of Earth System Science, 98(1), 71–89. https://doi.org/10.1007/BF02880377.
Noa Tang, S. D., Ntsama Atangana, J., & Onana, V. L. (2020). Mineralogy and geochemistry of alluvial sediments from the Kadey plain, eastern Cameroon: implications for provenance, weathering, and tectonic setting. Journal of African Earth Sciences, 163, 103763. https://doi.org/10.1016/j.jafrearsci.2020.103763.
Ohta, T., & Arai, H. (2007). Statistical empirical index of chemical weathering in igneous rocks: a new tool for evaluating the degree of weathering. Chemical Geology, 240(3–4), 280–297. https://doi.org/10.1016/j.chemgeo.2007.02.017.
Oni, S. O., & Olatunji, A. S. (2017). Depositional environments signatures, maturity and source weathering of Niger Delta sediments from an oil well in southeastern Delta State, Nigeria. Eurasian Journal of Soil Science, 6(3), 259. https://doi.org/10.18393/ejss.297245.
Pandey, R. (2013). Evidences of active continental arc setting from Lesser and Higher Himalayan granitoids, Bhutan Himalaya. Journal of Earth Science and Climate Change, 4, 121.
Pettijohn, F. J., Potter, P. E., & Siever, R. (1972). Sand and sandstone. Plate motions inferred from major element chemistry of lutites. Precambrian Research, 147, 124–147.
Potter, P. E. (1978). Petrology and chemistry of modern big river sands. The Journal of Geology, 86(4), 423–449.
Price, J. R., & Velbel, M. A. (2003). Chemical weathering indices applied to weathering profiles developed on heterogeneous felsic metamorphic parent rocks. Chemical Geology, 202(3–4), 397–416. https://doi.org/10.1016/j.chemgeo.2002.11.001.
Rahman, M. M., Arya, D. S., Goel, N. K., & Dhamy, A. P. (2011). Design flow and stage computations in the Teesta River, Bangladesh, using frequency analysis and MIKE 11 modeling. Journal of Hydrologic Engineering, 16(2), 176–186. https://doi.org/10.1061/(ASCE)HE.1943-5584.0000299.
Rahman, M. J. J., & Suzuki, S. (2007). Geochemistry of sandstones from the Miocene Surma Group, Bengal Basin, Bangladesh: implications for provenance, tectonic setting and weathering. Geochemical Journal, 41(6), 415–428. https://doi.org/10.2343/geochemj.41.415.
Ramesh, R., Ramanathan, A. L., Ramesh, S., Purvaja, R., & Subramanian, V. (2000). Distribution of rare earth elements and heavy metals in the surficial sediments of the Himalayan river system. Geochemical Journal, 34(4), 295–319. https://doi.org/10.2343/geochemj.34.295.
Ranjan, N., & Banerjee, D. M. (2009). Central Himalayan crystallines as the primary source for the sandstone–mudstone suites of the Siwalik Group: new geochemical evidence. Gondwana Research, 16(3–4), 687–696. https://doi.org/10.1016/j.gr.2009.07.005.
Reimann, K. U., & Hiller, K. (1993). Geology of Bangladesh. Berlin: Gebruder Borntraeger.
Roser, B. P., Cooper, R. A., Nathan, S., & Tulloch, A. J. (1996). Reconnaissance sandstone geochemistry, provenance, and tectonic setting of the lower Paleozoic terranes of the West Coast and Nelson, New Zealand. New Zealand Journal of Geology and Geophysics, 39(1), 1–16. https://doi.org/10.1080/00288306.1996.9514690.
Roser, B. P., & Korsch, R. J. (1986). Determination of tectonic setting of sandstone-mudstone suites using SiO2 content and K2O/Na2O ratio. The Journal of Geology, 94(5), 635–650. https://doi.org/10.1086/629071.
Roser, B. P., & Korsch, R. J. (1988). Provenance signatures of sandstone-mudstone suites determined using discriminant function analysis of major-element data. Chemical Geology, 67(1–2), 119–139. https://doi.org/10.1016/0009-2541(88)90010-1.
Roy, D. K., & Roser, B. P. (2013). Geochemical evolution of the Tertiary succession of the NW shelf, Bengal basin, Bangladesh: Implications for provenance, paleoweathering and Himalayan erosion. Journal of Asian Earth Sciences, 78, 248–262. https://doi.org/10.1016/j.jseaes.2013.04.045.
Sarin, M. M., Krishnaswami, S., Dilli, K., Somayajulu, B. L. K., & Moore, W. S. (1989). Major ion chemistry of the Ganga-Brahmaputra river system: Weathering processes and fluxes to the Bay of Bengal. Geochimica et Cosmochimica Acta, 53(5), 997–1009. https://doi.org/10.1016/0016-7037(89)90205-6.
Sharma, A., & Rajamani, V. (2000). Weathering of gneissic rocks in the upper reaches of Cauvery river, south India: implications to neotectonics of the region. Chemical Geology, 166(3–4), 203–223. https://doi.org/10.1016/S0009-2541(99)00222-3.
Singh, M., Sharma, M., & Tobschall, H. J. (2005). Weathering of the Ganga alluvial plain, northern India: implications from fluvial geochemistry of the Gomati River. Applied Geochemistry, 20(1), 1–21. https://doi.org/10.1016/j.apgeochem.2004.07.005.
Singh, P. (2010). Geochemistry and provenance of stream sediments of the Ganga River and its major tributaries in the Himalayan region India. Chemical Geology, 269(3–4), 220–236. https://doi.org/10.1016/j.chemgeo.2009.09.020.
Tandon, S. K., & Gupta, N. (2020). Introduction to geodynamics of the Indian plate: evolutionary perspectives. Cham: Springer. https://doi.org/10.1007/978-3-030-15989-4_1.
Taylor, S. R., & McLennan, S. M. (1985). The continental crust: its composition and evolution. Oxford: Blackwell Scientific Publications.
Thakur, V. C. (2013). Active tectonics of Himalayan frontal fault system. International Journal of Earth Sciences, 102(7), 1791–1810. https://doi.org/10.1007/s00531-013-0891-7.
Verma, S. P., & Armstrong-Altrin, J. S. (2013). New multi-dimensional diagrams for tectonic discrimination of siliciclastic sediments and their application to Precambrian basins. Chemical Geology, 355, 117–133. https://doi.org/10.1016/j.chemgeo.2013.07.014.
Viers, J., Dupré, B., & Gaillardet, J. (2009). Chemical composition of suspended sediments in World Rivers: New insights from a new database. Science of the Total Environment, 407(2), 853–868. https://doi.org/10.1016/j.scitotenv.2008.09.053.
von Eynatten, H., & Gaupp, R. (1999). Provenance of Cretaceous synorogenic sandstones in the Eastern Alps: constraints from framework petrography, heavy mineral analysis and mineral chemistry. Sedimentary Geology, 124(1–4), 81–111. https://doi.org/10.1016/S0037-0738(98)00122-5.
Whitney, D. L., & Evans, B. W. (2010). Abbreviations for names of rock-forming minerals. American Mineralogist, 95(1), 185–187. https://doi.org/10.2138/am.2010.3371.
Wronkiewicz, D. J., & Condie, K. C. (1987). Geochemistry of Archean shales from the Witwatersrand Supergroup, South Africa: source-area weathering and provenance. Geochimica et Cosmochimica Acta, 51(9), 2401–2416. https://doi.org/10.1016/0016-7037(87)90293-6.
Xie, Y., Yuan, F., Zhan, T., Kang, C., & Chi, Y. (2018). Geochemical and isotopic characteristics of sediments for the Hulun Buir Sandy Land, northeast China: implication for weathering, recycling and dust provenance. CATENA, 160, 170–184. https://doi.org/10.1016/j.catena.2017.09.008.
Acknowledgements
The authors would like to acknowledge Sudeb Chandra Das for his instructive comments in data analyzing, and the IMMM staff for their valuable contribution in sample collection and obtaining data in the lab. We would like to express our special acknowledgment to Priyadarsi D. Roy for his constructive and valuable reviews to enhance the quality of the manuscript. Finally, we would like to thank Mst. Arifa Akter for her cordial support offering imperative suggestions to build up the manuscript.
Funding
No funding was received for conducting this study.
Author information
Authors and Affiliations
Corresponding author
Ethics declarations
Conflicts of interest
The authors have no conflicts of interest to declare that are relevant to the content of this article.
Additional information
Communicated by M. V. Alves Martins.
Publisher's Note
Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
Supplementary Information
Below is the link to the electronic supplementary material.
Supplementary file 1: Online Resource 1
Mineralogical weight percentage in the bulk sediments of the Dharla River.
Supplementary file 2: Online Resource 2
Major element (in wt%) and trace element (in ppm) compositions along with CIA (Chemical index of alteration), PIA (Plagioclase index of alteration), W (Source rock weathering index), ICV (Index of compositional variability), and element ratios of the Dharla River sediments.
Supplementary file 3: Online Resource 3
Rare earth elements (REE; in ppm) composition and element ratios of the Dharla River sediments.
Supplementary file 4: Online Resource 4
Pearson’s correlation matrix using geochemical parameters of clastic sediment collected from the different locations along the Dharla River.
Rights and permissions
About this article
Cite this article
Rahman, M.M., Hasan, M.F., Hasan, A.S.M.M. et al. Chemical weathering, provenance, and tectonic setting inferred from recently deposited sediments of Dharla River, Bangladesh. J. Sediment. Environ. 6, 73–91 (2021). https://doi.org/10.1007/s43217-020-00046-z
Received:
Revised:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s43217-020-00046-z