Physico-chemical characteristics of Jharkhand and West Bengal thermal springs along SONATA mega lineament, India

Article

Singh, Hemant K., Chandrasekharam, D., Vaselli, O., Trupti, G., Singh, B., Lashin, Aref and Al Arifi, Nassir. 2015. "Physico-chemical characteristics of Jharkhand and West Bengal thermal springs along SONATA mega lineament, India." Journal of Earth System Science. 124 (2), pp. 419-430. https://doi.org/10.1007/s12040-015-0550-4
Article Title

Physico-chemical characteristics of Jharkhand and West Bengal thermal springs along SONATA mega lineament, India

ERA Journal ID1071
Article CategoryArticle
AuthorsSingh, Hemant K. (Author), Chandrasekharam, D. (Author), Vaselli, O. (Author), Trupti, G. (Author), Singh, B. (Author), Lashin, Aref (Author) and Al Arifi, Nassir (Author)
Journal TitleJournal of Earth System Science
Journal Citation124 (2), pp. 419-430
Number of Pages12
Year2015
Place of PublicationIndia
ISSN0253-4126
0973-774X
Digital Object Identifier (DOI)https://doi.org/10.1007/s12040-015-0550-4
Web Address (URL)https://link.springer.com/article/10.1007%2Fs12040-015-0550-4
Abstract

The chemical and isotopic compositions of thermal springs located along the Son–Narmada–Tapti (SONATA) mega lineament in central India have been investigated. The issuing temperatures of the thermal waters vary from 31° to 89°C for the thermal springs and 24° to 25°C for the cold springs. These thermal springs are located on the Archean Chotanagpur Gneissic Complex (CGC) in the eastern part of peninsular India. The thermal springs are mostly alkaline in nature with pH varying from 7.5 to 9.5. Piper diagram suggests that the chemistry of the thermal waters is compatible with the granitic host rocks through which the waters circulate. Mineral saturation index suggests that the thermal waters are saturated with cristobalite and quartz at lower temperatures (less than ∼130 to 150°C), and calcite and forsterite at higher temperatures (∼160° to 250°C). The estimated reservoir temperature based on chemical geothermometers is in the range of 132°–265°C, which favours a medium enthalpy geothermal system. Oxygen isotope fractionation of Bakreswar and Tantloi thermal springs highlights a higher reservoir temperature than estimated by chemical geothermometer. Positive gravity anomalies over Bakreswar and Tantloi areas strongly suggest a basement/mantle upliftment or mafic intrusion which could account for the heat source close to the surface. However, the large negative gravity anomaly depression around the Surajkund and Katkamsandi thermal springs indicates presence of deep seated faults.

KeywordsHazaribagh thermal spring, Bakreswar and Tantloi thermal spring, geochemistry of thermal spring
ANZSRC Field of Research 2020419999. Other environmental sciences not elsewhere classified
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Byline AffiliationsIndian Institute of Technology, India
University of Florence, Italy
King Saud University, Saudi Arabia
Institution of OriginUniversity of Southern Queensland
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