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Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/3872
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| Title: | The 3He/4He Halo of the Kazbek Volcanic Center, Northern Caucasus |
| Authors: | Lavrushin, V.* Polyak, B.* Strizhov, V. P.* Italiano, F.* Rizzo, A.* |
| Keywords: | helium isotopes Kazbek |
| Issue Date: | 2007 |
| Publisher: | Pleiades Publishing |
| Title of journal: | Doklady Earth Sciences |
| Series/Report no.: | 4/414 (2007) |
| Abstract: | Manifestations of recent volcanism in the Greater
Caucasus are grouped in the El’brus and Kazbek volcanic
areas [1]. The last episodes of activity in the majority
of their eruptive centers date back to the Late
Holocene or even first centuries of the recent era
(El’brus Volcano) [2]. This implies potential volcanic
hazards in the Greater Caucasus. Therefore, it is important
to outline contours of this potentially hazardous
region with the maximal possible accuracy. The region
is characterized by indications of geodynamic stress,
such as recent eruptions, crustal deformations, seismic
activity, geothermal anomalies, and others. The 3He/4He value in natural gases can serve as one of such
indications. |
| URI: | http://hdl.handle.net/2122/3872 |
| DOI: | 10.1134/S1028334X07040253 |
| Appears in Collections: | Papers Published / Papers in press 05.02.01. Geochemical data
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