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  1. University of Mandalay
  1. University of Mandalay
  2. Department of Physics

Hydrochemical and isotopic features of the Khaung Daing hot spring (Inle lake, Southern Shan State, Myanmar)

http://hdl.handle.net/20.500.12678/0000005184
1eb175b6-7ec3-41b1-8680-426cbdc4a2a4
bb8aeed0-6401-416b-8fd5-07a22bfa85c2
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Hydrochemical Hydrochemical and isotopic features of the Khaung Daing hot.pdf (337 Kb)
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Publication type Journal article
Upload type Publication
Title
Hydrochemical and isotopic features of the Khaung Daing hot spring (Inle lake, Southern Shan State, Myanmar)
en
Publication date 2017-09-04
Authors
Sacchi, Elisa
Re,Viviana
Setti,Massimo
Myat Mon Thin
Sipio,Eloisa Di
Description
The Inle lake watershed develops along a right-lateral strike-slip fault running parallel to the Sangaing fault, a major continental transform fault between the India and Sunda Plates. Located on the northwestern border of the Inle lake basin, the Khaung Daing hot spring outflows at a temperature of about 70°C. This contribution represents a reconnaissance study of the spring and describes its main hydrochemical and isotopic features, compared to surface and ground waters in the watershed. The water pH is slightly acidic, and, compared to the other water samples from the watershed, shows an EC in the high range (57-1284 μS/cm), the lowest pH and Eh values, and is Na-HCO3, whereas surface and ground waters are Ca(Mg)-HCO3 type. The hot spring isotopic composition falls close to the Yangon Meteoric Water Line, indicating that, despite its temperature, it is not strongly modified by water-rock interaction processes. Preliminary results suggest that this hydrothermal water is likely related to deep meteoric and ground water circulation within a fault zone, in a region characterized by an elevated geothermal gradient.
Keywords
Groundwater
Keywords
stable isotopes
Keywords
hydrothermal waters
Keywords
mineralogy
Journal articles
Procedia Earth and Planetary Science
750 – 753
17
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