Mukerji, P. (1999) A brief description on radon monitoring in India in some seismically sensitive areas. Il nuovo cimento C, 22 C (3-4). pp. 509-522. ISSN 1826-9885
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Abstract
Radon anomalies in both groundwater as well as soil gas prior to a major earthquake were first observed in the Tashkent region (1966) of USSR. Since then, scientists have taken note of geochemical changes in seismically active areas on a regular basis. Emanation of radon gases and associated anomalies in spring and well waters have been observed in various seismically active regions in the Himalayan belt — both in the north-eastern as well as in the western part of the mountain chain. An attempt has been made in this paper to give a brief review of the radon monitoring work done in the Indian subcontinent in some seismically active regions.
| Item Type: | Article |
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| Additional Information: | Paper presented at the “Fourth International Conference on Rare Gas Geochemistry”, Rome, October 8-10, 1997. |
| Uncontrolled Keywords: | Volcanology; radiation detectors; viscosity, diffusion, and thermal conductivity |
| Subjects: | 500 Scienze naturali e Matematica > 550 Scienze della Terra > 551 Geologia, Idrologia, Meteorologia > 551.9 Geochimica |
| Depositing User: | Marina Spanti |
| Date Deposited: | 11 Oct 2019 12:52 |
| Last Modified: | 11 Oct 2019 12:52 |
| URI: | http://eprints.bice.rm.cnr.it/id/eprint/13458 |
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