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The Mayskoye disseminated gold deposit, Chukotka, Russia: mineral paragenesis, fluid inclusion, and oxygen and sulfur isotope studiesстатья
Информация о цитировании статьи получена из
Web of Science,
Scopus
Дата последнего поиска статьи во внешних источниках: 19 июля 2013 г.
- Авторы: Bortnikov N.S., Prokof’ev V.Yu, Vikentieva O.V., Bryzgalov I.A., Krivitskaya N.N.
- Сборник: Mineral Exploration and Sustainable Development
- Том: 1
- Год издания: 2003
- Место издания: Netherlands Athens, Greece Millpress Roterdam
- Первая страница: 743
- Последняя страница: 746
- DOI: WOS:000221378600184
- Аннотация: New data on mineral paragenesis, mineral chemistry, fluid inclusions, oxygen isotopes of quartz, and sulfur isotope compositions of sulfide minerals from the black shale-hosted Mayskoye disseminated gold deposit are presented. Three distinct mineralization stages include: (1) disseminated sulfide minerals, (2) wolframite-cassiterite-quartz veins, and (3) quartz-stibnite veins. Several compositionally and isotopically distinct fluids were involved in the Mayskoye hydrothermal system. Both unmixed into a low salinity, H2O+CO2+CH4 liquid and a CO2+ H2O vapor-rich phase, with economic disseminated gold ores deposited at 238degrees-430degreesC and 0.2 to 1.2 kbar.
- Добавил в систему: Прокофьев Всеволод Юрьевич