Recharge Conditions of the Low Temperature Paratunsky Geothermal Reservoir, Kamchatka, Russia

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• 作者：A.V. Kiryukhin^a ; ^{AVKiryukhin2@mail.ru} ; N.P. Asaulova^b ; L.A. Vorozheikina^b ; N.V. Obora^b ; P.O. Voronin^a ; E.V. Kartasheva^a
• 关键词：Paratunsky ; recharge ; geothermal ; reservoir
• 刊名：Procedia Earth and Planetary Science
• 出版年：2017
• 出版时间：2017
• 年：2017
• 卷：17
• 期：Complete
• 页码：132-135
• 全文大小：280 K
• 卷排序：17

文摘

The Paratunsky geothermal field is a classic example of a low temperature hydrothermal reservoir of meteoric origin. Hydrogeochemical zoning reflects a different intensity of water exchange in the Western and Eastern sites of the field. The hydrogeochemical history of operations 1966-2015 shows the involvement of chloride waters across the field's Eastern boundary. Water recharge to the Paratunsky geothermal field is provided mostly by meteoric waters from elevations above +1150 masl. The most likely area of water recharge to the Paratunsky geothermal fields is the Vilyuchinsky volcano (elevation 2173 m abs.).