Криометрические и термометрические исследования флюидных включений в кварце золоторудного месторождения Балка Широкая
The investigation of fluid inclusions for the gold deposit shows the evolution of the regres-sive mineral-forming system in the completed geological cycle. At the beginning of the cycle, the metamorphism destroyed inclusions of the volcanic stage and formed a new system of high-temperature inclusi...
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| Date: | 2008 |
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| Main Authors: | , , , |
| Format: | Article |
| Language: | Russian |
| Published: |
Видавничий дім "Академперіодика" НАН України
2008
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| Subjects: | |
| Online Access: | https://nasplib.isofts.kiev.ua/handle/123456789/4128 |
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| Journal Title: | Digital Library of Periodicals of National Academy of Sciences of Ukraine |
| Cite this: | Криометрические и термометрические исследования флюидных включений в кварце золоторудного месторождения Балка Широкая / Ю.А. Фомин, М.О. Витык, Ю.Н. Демихов, Е.Е. Лазаренко // Доп. НАН України. — 2008. — № 3. — С. 122-127. — Бібліогр.: 6 назв. — рос. |
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Digital Library of Periodicals of National Academy of Sciences of Ukraine| Summary: | The investigation of fluid inclusions for the gold deposit shows the evolution of the regres-sive mineral-forming system in the completed geological cycle. At the beginning of the cycle,
the metamorphism destroyed inclusions of the volcanic stage and formed a new system of
high-temperature inclusions rich in CO2 and CH4. The next tectonic-metasomatic activity
transformed the system to the epithermal one revealed by rich liquid inclusions with gas and,
sometimes, solid phases.
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| ISSN: | 1025-6415 |