Formation of gold mineralization in ultramafic alkalic magmatic complexes
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https://elib.sfu-kras.ru/handle/2311/33042Дата:
2016-06Журнал:
Doklady Earth SciencesКвартиль журнала в Scopus:
Q2Квартиль журнала в Web of Science:
Q4Библиографическое описание:
Ryabchikov, I. D. Formation of gold mineralization in ultramafic alkalic magmatic complexes [Текст] / I. D. Ryabchikov, L. N. Kogarko, A. M. Sazonov, N. N. Kononkova // Doklady Earth Sciences. — 2016. — Т. 468 (№ 2). — С. 623-625Текст статьи не публикуется в открытом доступе в соответствии с политикой журнала.
Аннотация:
Study of mineral inclusions within alluvial gold particles of the Guli Complex (East Siberia) and findings of lode gold in rocks of the same intrusion have demonstrated that gold mineralization occurs in interstitions of both early high–magnesium rocks (dunite) and later alkalic and carbonatite rocks. In dunite the native gold occurs in association with Fe–Ni sulfides (monosulfide solid solution, pentlandite, and heazlewoodite). Formation of the gold-bearing alloys took place under a low oxygen potential over a broad range of temperatures: from those close to 600°C down to below 400°C. © 2016, Pleiades Publishing, Ltd.