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Palaeoweathering, Tectonic Setting and Climatic Condition of Sabarmati Alluvial Plain in Ahmadabad City, Gujarat, Western India

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Abstract

The present study emphasizes major elemental geochemical attributes-based prediction of nature, palaeoweathering intensity, provenance, tectonic setting and palaeoclimatic condition of source area of Sabarmati alluvial sediments lying in Ahmadabad locality, Gujarat, India. The sediments successions are comprised of gravel, poorly graded sand, with dominant silty and clayey sands, silt and clay with low-to-high level of plasticity. The sediments exhibit increasing concentration of MnO followed by P2O5, TiO2, K2O, MgO, Na2O, CaO, Fe2O3, Al2O3 and SiO2 which supports quartz dominating sand layers in comparison with silty and clayey sequences. The values of SiO2/Al2O3, Na2O/Al2O3 and K2O/Al2O3 and higher values of ICV indicate immature sediments with low dilution of ‘Na’ and ‘K’. Lithologically, the majority of sediments belong to shale and Fe-shale varieties. The values of ICV, CIA, CIW and PIA and various bivarient and discrimination diagrams reveal the mechanical fragmentation, abrasion and low to moderate degree of chemical palaeoweathering of fragments of felsic and intermediate igneous rocks of rift basin located at island arch and active continental margin under arid/semi-arid conditions sporadically interfered by short-term humid and semi-humid climatic conditions were responsible for formation of sediments sequences of the area.

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References

  1. Dupre B, Dessert C, Oliva P, Godderis Y, Viers J, François L, Millot R, Gaillardet J (2003) Rivers, chemical weathering and Earth’s climate. C R Geosci 335:1141–1160

    Article  CAS  Google Scholar 

  2. Fedo CM, Nesbitt HW, Young GM (1995) Unravelling the effects of potassium metasomatism in sedimentary rocks and paleosols, with implications for paleoweathering conditions and provenance. Geology 23:921–924

    Article  ADS  CAS  Google Scholar 

  3. Nesbitt HW, Young GM (1984) Prediction of some weathering trends of plutonic and volcanic rocks based on thermodynamic and kinetic considerations. Geochim Cosmochim Acta 48:1523–1534

    Article  ADS  CAS  Google Scholar 

  4. Harnois L (1988) The CIW index: a new chemical index of weathering. Sediment Geol 55:319–322

    Article  ADS  CAS  Google Scholar 

  5. Cox R, Lower DR, Cullers RL (1995) The influence of sediment recycling and basement composition on evolution of mud rock chemistry in the southwestern United States. Geochem Cosmochim Acta 59:2919–2940

    Article  ADS  CAS  Google Scholar 

  6. Herron MM (1986) Geochemical classification of terrigeneous sands and shales from core or log data. J Sediment Petrol 58:820–829

    Google Scholar 

  7. Moosavirad SM, Janardhana MR, Sethumadhav MS, Moghadam MR, Shankara M (2010) Geochemistry of lower Jurassic shales of the Shemshak Formation, Kerman Province, Central Iran: provenance, source weathering and tectonic setting. Chem Erde-Geochem 71:279–288

    Article  ADS  Google Scholar 

  8. Servaraj K, Arthur CC (2006) Moderate chemical weathering of subtropical Taiwan, constraints from solid-phase geochemistry of sediments and sedimentary rocks. J Geol 114:101–116

    Article  ADS  Google Scholar 

  9. Amajor LC (1987) Major and trace elements geochemistry of Albin and Touronian shales from the Southern Benue trough, Nigeria. J Afr Earth Sci 6:633–641

    CAS  Google Scholar 

  10. Roser BP, Korsch RJ (1988) Provenance signatures of sandstone-mudstone suites determined using discriminant function analysis of major-element data. Chem Geol 67:119–139

    Article  ADS  CAS  Google Scholar 

  11. Suttner LJ, Dutta PK (1986) Alluvial sandstones and paleoclimate framework mineralogy. J Sediment Petrol 56:329–345

    CAS  Google Scholar 

Download references

Acknowledgements

The authors are grateful to Dr. M. Ravi Kumar, Director General, Institute of Seismological Research, ISR Gandhinagar, Gujarat, India, for his kind support and encouragement for doing this research work and providing facilities of XRF analysis. The authors are thankful to Mr. Gyan Prakash Satyam, JRF, UGC-CSIR, IIT(ISM), Dhanbad, for his drawing and supportive works. The authors are thankful to Prof. B.C. Sarkar, Department of Applied Geology, IIT(ISM), Dhanbad, India, for his inspiration and providing necessary facility in preparation of present work. The help and cooperation of Shri Anubhav Sukla, IIT (ISM), Dhanbad, is thankfully acknowledged. Authors are also grateful to Prof. B. K. Rastogi, ISR, for his kind support, valuable suggestions and encouragement for doing this work. The study was supported by the Ministry of Earth Science under the Project MoES No. 115/IFD/15) and DAE-BRNS, Mumbai, India (File No. 2013/36/56-BRNS/2447).

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Dubey, R.K., Dwivedi, V.K. Palaeoweathering, Tectonic Setting and Climatic Condition of Sabarmati Alluvial Plain in Ahmadabad City, Gujarat, Western India. Natl. Acad. Sci. Lett. 44, 21–25 (2021). https://doi.org/10.1007/s40009-020-00953-9

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  • DOI: https://doi.org/10.1007/s40009-020-00953-9

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