Induced seismicity due to the oil production in  Tbilisi region, Georgia

Chelidze, T.; Jimsheladze, T.; Melikadze, G.

Please use this identifier to cite or link to this item: http://openlibrary.ge/handle/123456789/4857

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DC Field	Value	Language
dc.contributor.author	Chelidze, T.	en_US
dc.contributor.author	Jimsheladze, T.	en_US
dc.contributor.author	Melikadze, G.	en_US
dc.date.accessioned	2015-01-16T11:02:10Z	-
dc.date.available	2015-01-16T11:02:10Z	-
dc.date.issued	2010	-
dc.identifier.citation	Research workshop on Exploration and Exploitation of Groundwater and Thermal Water Systems in Georgia. Tbilisi, Georgia 2010, pp.83-95	en_US
dc.identifier.uri	http://hdl.handle.net/123456789/4857	-
dc.description.abstract	30 km to the north-east from the Tbilisi hydrothermal field (THF) the oil field has been revealed. The intensive oil production in 80-s disturbs the regime of the central hydrothermal deposit and causes depletion and desalination of springs. Later on, after cessation of intensive extraction, the regime of hydrothermal field was recovered. These facts point to the significant change of pore pressure conditions during oil production process and triggered an idea to analyze the seismic activity in the period of oil production. As it is well known that the pore pressure change may provoke changes in the seismic activity (Gupta and Rastogi, 1976, Grasso and Sornette, 1998) the attempt is made to assess seismic effects induced by the oil production in the THF.	en_US
dc.language.iso	en	en_US
dc.subject	გეოფიზიკა	ka_Ge
dc.subject	შრომები	ka_Ge
dc.subject	Induced Seismicity	en_US
dc.subject	Oil production	en_US
dc.title	Induced seismicity due to the oil production in Tbilisi region, Georgia	en_US
dc.type	Article	en_US
dc.date.published	2010	-
Appears in Collections:	შრომები - Труды - Articles

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