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<article language="en">
	<journal>
		<journal_title>eEarth Discussions</journal_title>
		<journal_url>www.electronic-earth-discuss.net</journal_url>
		<issn>1815-3836</issn>
		<eissn>1815-3844</eissn>
		<volume_number>4</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/eed-4-77-2009</doi>
	<article_url>http://www.electronic-earth-discuss.net/4/77/2009/</article_url>
	<abstract_html>http://www.electronic-earth-discuss.net/4/77/2009/eed-4-77-2009.html</abstract_html>
	<fulltext_pdf>http://www.electronic-earth-discuss.net/4/77/2009/eed-4-77-2009.pdf</fulltext_pdf>
	<start_page>77</start_page>
	<end_page>89</end_page>
	<publication_date>2009-09-29</publication_date>
	<article_title content_type="html">Thermogeodynamic manifestations in the Caucasus and their genesis</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>G. E. Gugunava</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>J. K. Kiria</name>
		</author>
		<author numeration="3" affiliations="1,2">
			<name>T. B. Bochorishvili</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute of Geophysics, Georgian Academy of Sciences, Rukhadze St 1, 0193 Tbilisi, Georgia</affiliation>
		<affiliation numeration="2" content_type="html">Institute of Informatics, University of Podlasie, 3-go Maja 54, 08-110 Siedlce, Poland</affiliation>
	</affiliations>
	<abstract content_type="html">In the work two aspects of thermal character are considered: first of all
this is the connection of subduction phenomena with thermal life of the
Caucasus on the basis of over interpreted data of magnetotelluric sounding,
and secondly, origin of thermostressed condition of the Caucasus and its
geological aspects which is manifested in the following:
&lt;br&gt;&lt;br&gt;
1.  in the zones of anomalous thermodisplacements thermofaults should occur
(Le Pishon et al., 1977). These thermofaults are in good correlation with deep faults
which are distinguished by geological and seismic methods, these thermofaults may be
earthquake sources (Spitak, Racha, etc. earthquakes), also may be channels through
which magma derivates (giving mineral deposits) may penetrate on surface (Gugunava and Gijeishvili, 1989);
&lt;br&gt;&lt;br&gt;
2.  in the body of sedimentary complex thermostressed seals and seal failures occur,
which are apparently traps for oil-gas fluids. Good correlation of thermodense anomalies
with oil deposits of the Caucasus is shown (Alexidze et al., 1985; Gugunava,
1980).
&lt;br&gt;&lt;br&gt;
Everything above mentioned was carried out within frames of stationary
thermal model which did not allow us to reveal time characteristics of
interconnection of geological medium and thermal field.
&lt;br&gt;&lt;br&gt;
Now investigations are being carried out within the frames of stationary
thermal model and its interconnection with geological environment.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Alexidze M. A., Gugunava, G. E., Kiria, J. K., and Chelidze, T. L.: Thermal model, crustal inversional layer and young volcanism of the Caucasus, Bulletin of the Georgian Academy of Sciences, 113, 517–521, 1985. </reference>
		<reference numeration="2" content_type="text"> Alexidze, M. A., Gugunava, G. E., Kiknadze, D. A., Kiria, J. K., and Chelidze, T. L.: Geothermal model of the Caucasus and crustal astenosphere, in: Proceedings of the International Conference on Gepthermal Model of Geological Structures and Crustal Astenosphere, St-Peterburg, Russia, 91–96, September 1991. </reference>
		<reference numeration="3" content_type="text"> Alexidze, M. A., Gugunava, G. E., Kiria, J. K., and Chelidze, T. L.: A three-dimensional geothermal stationary model of thermal and thermoelastic fields of Caucasus Erratum, Tectonophysics, 227, 191–203, 1993. </reference>
		<reference numeration="4" content_type="text"> Gugunava, G. E.: On construction of geoelectric model of the upper mantle of the Caucasus, Bulletin of the Georgian Academy of Sciences, 100, 89–92, 1980. </reference>
		<reference numeration="5" content_type="text"> Gugunava G. E. and Gijeishvili S. O.: About possible thermoelastic nature of Spitak earthquake, Thesis in: regional conf. Sverdlovsk, Russia, 44~pp., 1989. </reference>
		<reference numeration="6" content_type="text"> Gugunava, G. E.: On thermoelastic mechanism of oil-gas migration, Bulletin of the Georgian Academy of Sciences, 150, 58–63, 1994. </reference>
		<reference numeration="7" content_type="text"> Gugunava, G. E.: On thermoelastic mechanisms of genesis of oil fields region and method of their reveal, Journal of Georgian Geophysics Society Issue (A), Physics of solid earth, 1, 116–119, 1995. </reference>
		<reference numeration="8" content_type="text"> Gugunava, G. E., Kiria, J. K., Gogiashvili, J. V., and Kiknadze, D. A.: On genesis of Shamkori, Spitak and Racha-Java earthquakes, Journal of the Georgian Geophysical Society Issue (A), 11, 63–68, 2006. </reference>
		<reference numeration="9" content_type="text"> Hain, V. N.: Regional geotectonics (Alpine Mediterranean Belt), Nedra, Moscow, 181–188, 1984. </reference>
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	</references>
</article>

