Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4458543 | Journal of Geochemical Exploration | 2006 | 6 Pages |
Abstract
Among the thermal waters of Mendeleev Volcano three main types can be distinguished: sodium-chloride, acid-sulfate and chloride–sulfate–bicarbonate waters. Contents and behaviors of siderophile, chalcophile, lithophile, and rare-earth elements are discussed. These data, together with the result of isotopic studies (oxygen and hydrogen), are used to discuss the origin of these waters. From the three types of thermal waters, only acid-sulfate waters have a significant input on the chemical composition of the surrounding surface waters.
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Authors
O. Chudaev, V. Chudaeva, K. Sugimori, A. Kuno, M. Matsuo,