Тип публикации: статья из журнала

Год издания: 2021

Идентификатор DOI: 10.3390/min11040354

Ключевые слова: alkaline and carbonatite magmatism, carbonaceous-au-pgm ore formation, ultramafic

Аннотация: The gold and platinum-group elements (PGE) mineralization of the Guli and Kresty intrusions was formed in the process of polyphase magmatism of the central type during the Permian and Triassic age. It is suggested that native osmium and iridium crystal nu

Журнал: Minerals

Выпуск журнала: Vol. 11, Is. 4

Номера страниц: 354

ISSN журнала: 2075163X

Издатель: MDPI AG

• Sazonov A.M. (Department of Geology, Mineralogy and Petrography, Siberian Federal University, Krasnoyarsk, 660041, Russian Federation)
• Romanovsky A.E. (Department of Geology, Mineralogy and Petrography, Siberian Federal University, Krasnoyarsk, 660041, Russian Federation)
• Gertner I.F. (Department of Geology and Geography, Tomsk State University, Tomsk, 634050, Russian Federation)
• Zvyagina E.A. (Department of Geology, Mineralogy and Petrography, Siberian Federal University, Krasnoyarsk, 660041, Russian Federation)
• Krasnova T.S. (Department of Geology and Geography, Tomsk State University, Tomsk, 634050, Russian Federation)
• Grinev O.M. (Department of Geology and Geography, Tomsk State University, Tomsk, 634050, Russian Federation)
• Silyanov S.A. (Department of Geology, Mineralogy and Petrography, Siberian Federal University, Krasnoyarsk, 660041, Russian Federation)
• Kolmakov Y.V. (Department of Geology and Geophysics, Tomsk Polytechnic University, Tomsk, 634050, Russian Federation)

• Scopus
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