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Role of Hydrothermal Fluids in the Deterioration of Pictographs and Petroglyphs in Rock Shelters of The Gawilgarh Hills, Madhya Pradesh, India


Affiliations
1 Department of Geology, RTM Nagpur University, Nagpur 440 001, India
2 Department of Ancient History, Archaeology, and Culture, RTM Nagpur University, Nagpur 440 033, India
3 Geological Survey of India, Central Region, Seminary Hills, Nagpur 440 006, India
4 Archaeological Survey of India, Mumbai Circle, Sion (E), Mumbai 400 022, India
 

India has one of the largest concentrations of rock-art sites. However, these rock shelters have deteriorated due to natural agencies. The present study was carried out in one such site in Central India, which is hosted by argillaceous and ferruginous sandstones, showing pro-minent chemical, biological and mechanical weather-ing. The results based on field investigations, petrography, XRD, FE-SEM-EDS and FTIR meas-urements have indicated that chemical weathering is caused due to infiltration of hydrothermal fluids through innumerable zones of weaknesses formed due to neotectonic activities in the Satpura Lineament Zone, especially along Gawilgarh and Salbardi Faults in this region.

Keywords

Archeological Site, Chemical Weathering, Hydrothermal Fluids, Rock Shelters.
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  • Chakravarty, K. K. and Bednarik, R. G., Indian Rock Art and its Global Context. Amazon Bestsellers, 1997, p. 228; ISBN 8120814649.

  • UNESCO World Heritage Site, Rock Shelters of Bhimbetka, 1992–2020; http://whc.unesco.org/en/list/925 (accessed on 10 May 2020).

  • Kumar, G., Major rock art regions in India, 2015; https:// rockartweb.com/major-rock-art-regions-in-india (accessed on 10 May 2020).

  • Ingole, V., Lad, P., Khode, M., Damahe, D., Patil, S. and Hirurkar, P., Discovery of painted rock-shelters from Satpura–Tapti Valley. Purakala, 2007, 17, 153–158.

  • Godhal, V. and Shende, A., Reflection of the ecological aspect of animal depicted in rock art of Satpura–Tapti Valley and nearby region. In Puratattva, Indian Archeological Society, New Delhi, 2011, vol. 41, pp. 216–223.

  • Bhattacharya-Sahu, N. and Sahu, P., Decorated rock shelters of Gawilgarh Hills, District Betul, Madhya Pradesh. In Rock Art Studies – Concept, Methodology, Context, Documentation and Conservation (ed. Malla, B.), IGNCA and Aryan Books Interna-tional, New Delhi, 2014, pp. 271–298.

  • Bhattacharya-Sahu, N. and Sahu, P., Artistry in the rock shelters of Gawilgarh Hills: Recent Discoveries. In Puratattva, Indian Ar-chaeological Society, New Delhi, 2014, vol. 44, pp. 63–78.

  • Bhattacharya-Sahu, N. and Sahu, P., Rock art treasures of the Satpuras: Recent discoveries in the Gawilgarh Hills of Betul Dis-trict, Madhya Pradesh. In Rock Art in India in Felicitation of Prof. V. H. Sonawane (eds Pradhan, S. and Garnayak, D. B.), B. R. Pub-lishing Corporation, Delhi, 2017, pp. 103–113.

  • Bhattacharya-Sahu, N. and Sahu, P., Rock art of Gawilgarh Hills. In Puratattva, Indian Archaeological Society, New Delhi, 2017, vol. 47, pp. 63–78.

  • Bhattacharjee, D., Chattopadhyay, A. and Jain, V., Polyphase neo-tectonic movements in the Gavilgarh Fault zone, central Indian craton: evidences from geomorpho-tectonic analysis. Geophysical Research Abstracts, EGU2014-6482-1, 2014, 16; https:// repository.iitgn.ac.in/handle/123456789/1364 11. Chattopadhyay, A., Holdsworth, R. E., Sherlok, S. C. and Widdowson, M., Constraining the ages of polyphase fault reacti-vation of the Gavilgarh–Tan Shear zone, central India using la-serprobe 40Ar–39Ar dating of pseudotachylytes. In Tectonics Studies Group Meeting, Cardiff, UK, 2014.

  • Srivastava, A. K. and Mankar, R. S., Lithofacies, depositional environment and age of Salbardi area, Amravati district, Maha-rashtra and Betul, Madhya Pradesh. J. Geol. Soc. India, 2008, 72, 190–198.

  • Surendranath, M., Geomorphology of the Tapti Valley, Ph.D. dis-sertation, Indian Institute of Technology Bombay, 1984.

  • Venkatakrishnan, R., Parallel scarp retreat and drainage evolution, Pachmarhi area, Madhya Pradesh, central India. J. Geol. Soc. India, 1984, 25, 401–413.

  • Sheth, H. C. et al., Geology and geochemistry of Pachmarhi dykes and sills, Satpura Gondwana Basin, central India: problems of dyke-sill-flow correlations in the Deccan Traps. Contrib. Mineral. Petrol., 2009, 158, 357–380.

  • Ravi Shankar, Neotectonic activity along the Tapti–Satpura lineament in the Central India. Indian Miner., 1987, 41, 19–30.

  • Guha, S., Tectonic framework and evolution of the Tapi basin – an intracratonic half-graben from west-central India. Indian Miner., 1995, 49, 61–78.

  • Ray, R., Sheth, H. C. and Mallik, J., Structure and emplacement of the Nandurbar-Dhule mafic dyke swarm, Deccan Traps, and the tectonomagmatic evolution of flood basalts. Bull. Volcanol., 2007, 69, 537–551.

  • Saxena, V. I. and Gupta, M. L., Geochemistry of the thermal waters of Salbardi and Tatapani, India. Geothermics, 1986, 15, 705–714.

  • Srivastava, A. K. and Mankar, R. S., Trace fossils and their palaeo-environment significance in the Lameta Formation of Salbardi and Belkar area, district Amravati, Maharashtra. Saudi Soc. Geosci., 2011, 1–7.

  • Tucureanu, V., Matei, A. and Avram, A. M., FTIR spectroscopy for carbon family study. Crit. Rev. Anal. Chem., 2016, 46(6), 502–520.

  • MacLeod, I. D., Haydock, P. and Charton, E., Avian Guano and its Effects on the Preservation of Rock Paintings’ in Preservation of Rock Art, Occasional AURA Publication, 1996, vol. 9, pp. 60–64.

  • Clair, L. and Seaward, M. (eds), Biodeterioration of rock substrata by lichens: progress and problems. In Biodeterioration of Stone Surfaces: Lichens and Biofilms as Weathering Agents of Rocks and Cultural Heritage, Kluwer, Dordrecht, 2004, pp. 1–8.

  • Sarolkar, P., Exploration strategy for hot springs associated with gondwana coalfields in India. Proc. World Geother. Congr., 2010, 74.

  • Ravi Shanker, Geothermal regime in the Son–Narmada lineament zone. In Geoscientific Studies of the Son–Narmada–Tapti Linea-ment Zone, Geological Survey of India, 1995, pp. 213–248.

  • Randive, K. R., Chaudhary, S., Dandekar, S., Deshmukh, K., Peshwe, D., Dora, M. L. and Belyatski, B., Characterization and Genesis of Chalcedony Occurring within Deccan Traps Basaltic Lava Flows, LIT Hill, Nagpur City, India. J. Earth Syst. Sci., 2019, pp. 1–31.

  • Da Silva, Al, da Oliveira, A. H. and Fernandez, M. L. S., Influ-ence of preferred orientation of minerals in the mineralogical iden-tification process by X-ray diffraction. In International Nuclear Atlantic Conference – INAC 2011, Belo Horizonte, MG, Brazil, 2011; ISBN: 978-85-99141-04-5.


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  • Role of Hydrothermal Fluids in the Deterioration of Pictographs and Petroglyphs in Rock Shelters of The Gawilgarh Hills, Madhya Pradesh, India

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Authors

Kirtikumar Randive
Department of Geology, RTM Nagpur University, Nagpur 440 001, India
Prabash Sahu
Department of Ancient History, Archaeology, and Culture, RTM Nagpur University, Nagpur 440 033, India
Sanjeevani Jawadand
Department of Geology, RTM Nagpur University, Nagpur 440 001, India
Tushar Meshram
Geological Survey of India, Central Region, Seminary Hills, Nagpur 440 006, India
Sneha Dandekar
Department of Geology, RTM Nagpur University, Nagpur 440 001, India
Tejashree Raut
Department of Geology, RTM Nagpur University, Nagpur 440 001, India
Gunjan Saha
Department of Geology, RTM Nagpur University, Nagpur 440 001, India
M. L. Dora
Geological Survey of India, Central Region, Seminary Hills, Nagpur 440 006, India
Nandini Bhattacharya-Sahu
Archaeological Survey of India, Mumbai Circle, Sion (E), Mumbai 400 022, India

Abstract


India has one of the largest concentrations of rock-art sites. However, these rock shelters have deteriorated due to natural agencies. The present study was carried out in one such site in Central India, which is hosted by argillaceous and ferruginous sandstones, showing pro-minent chemical, biological and mechanical weather-ing. The results based on field investigations, petrography, XRD, FE-SEM-EDS and FTIR meas-urements have indicated that chemical weathering is caused due to infiltration of hydrothermal fluids through innumerable zones of weaknesses formed due to neotectonic activities in the Satpura Lineament Zone, especially along Gawilgarh and Salbardi Faults in this region.

Keywords


Archeological Site, Chemical Weathering, Hydrothermal Fluids, Rock Shelters.

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DOI: https://doi.org/10.18520/cs%2Fv121%2Fi2%2F255-263