Kovalenker, Vladimir A; Plotinskaya, Olga Yu (2005) Te and Se mineralogy of Ozernovskoe and Prasolovskoe epithermal gold deposits, Kuril–Kamchatka volcanic belt. Geochemistry, Mineralogy and Petrology (Sofia), 43. 118-124
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | Te and Se mineralogy of Ozernovskoe and Prasolovskoe epithermal gold deposits, Kuril–Kamchatka volcanic belt | ||
| Journal | Geochemistry, Mineralogy and Petrology (Sofia) | ||
| Authors | Kovalenker, Vladimir A | Author | |
| Plotinskaya, Olga Yu | Author | ||
| Year | 2005 | Volume | < 43 > |
| Page(s) | 118-124 | ||
| Publisher | Citeseer | ||
| Original Entry | Kovalenker, V.A., Plotinskaya, O.Yu. (2005): Te and Se mineralogy of Ozernovskoe and Prasolovskoe epithermal gold deposits, Kuril – Kamchatka volcanic belt. Geochemistry, Mineralogy and Petrology: 43: 118-123 | ||
| Classification | Not set | LoC | Not set |
| Mindat Ref. ID | 16065259 | Long-form Identifier | mindat:1:5:16065259:4 |
| GUID | 0 | ||
| Full Reference | Kovalenker, Vladimir A; Plotinskaya, Olga Yu (2005) Te and Se mineralogy of Ozernovskoe and Prasolovskoe epithermal gold deposits, Kuril–Kamchatka volcanic belt. Geochemistry, Mineralogy and Petrology (Sofia), 43. 118-124 | ||
| Plain Text | Kovalenker, Vladimir A; Plotinskaya, Olga Yu (2005) Te and Se mineralogy of Ozernovskoe and Prasolovskoe epithermal gold deposits, Kuril–Kamchatka volcanic belt. Geochemistry, Mineralogy and Petrology (Sofia), 43. 118-124 | ||
| In | Link this record to the correct parent record (if possible) | ||
| Abstract/Notes | We describe two epithermal telluride-selenide bearing Au-Ag deposits: Prasolovskoe and Ozernovskoe, both located within the Kuril-Kamchatka volcano-plutonic belt. Several rare and unknown Te and Se minerals were found at both deposits. At the Prasolovskoe deposit, various Te-Se minerals, including an unnamed Te3Se4 phase are widespread, while at the Ozernovskoe deposit selenides and sulfoselenides are typical. Te-Se mineralization at both deposits was formed in a rather narrow temperature interval (250- 200 oC); the composition of mineral assemblages was determined by activities of S2 , O2 , Te, and Se in the system. At early stages of ore-forming process, fluids were characterized by high aS2 . With temperature decrease, aS2 also decreased, resulting in aTe2 increase, and, later aSe2 increase. That caused at first an abundant sulfides precipitation, then the formation of tellurides, followed by the crystallization of selenotellurides, and, finally, selenides. | ||
Map of Localities
Locality Pages
Mineral Pages
| Mineral | Citation Details |
|---|---|
| UM1989-29-Se:Te | |
| Unnamed (Bi Telluride Selenide II) | |
| Unnamed (Bi Telluride Selenide III) | |
| Unnamed (Bi Telluride Selenide IV) | |
| Unnamed (Se-analogue of Pavonite) |
Mineral Occurrences
See Also
These are possibly similar items as determined by title/reference text matching only.
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