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The evolution of the ore-forming system in the low sulfide horizon of the Noril'sk 1 intrusion, Russiaстатья
Информация о цитировании статьи получена из
Web of Science
Статья опубликована в журнале из списка Web of Science и/или Scopus
Дата последнего поиска статьи во внешних источниках: 8 сентября 2021 г.
- Авторы: Tolstykh Nadezhda D., Zhitova Liudmila M., Shapovalova Maria O., Chayka Ivan F.
- Журнал: Mineralogical Magazine
- Том: 83
- Номер: 5
- Год издания: 2019
- Издательство: Mineralogical Society
- Местоположение издательства: United Kingdom
- Первая страница: 673
- Последняя страница: 694
- DOI: 10.1180/mgm.2019.47
- Аннотация: We present here new data on the low-sulfide mineralisation in the upper endocontact of the Noril'sk 1 intrusion. Twenty four mineral species of platinum-group elements and their solid solutions, as well as numerous unnamed phases, including an Sb analogue of vin-centite, As and Sn analogues of mertieite-I and a Sn analogue of mertieite-II have been found. It is shown that the features of the mineral association: (1) the atypical trend of TiO2 and Fe2+ in chromian spinet; (2) the composition of the Pt-Fe alloys with a Fe/Fe + Pt range of 0.26-0.37 (logf(O2), approximate to - (9-10); and (3) crystallisation of high-temperature sperrylite from silicate melt (at >800 degrees C and logf(S2) < -10.5), which is possible under f(O2) of FMQ to FMQ-2 in mafic magma, are due to the reducing conditions of their formation and evolution. Droplet-like inclusions of silicate-oxide minerals in chromian spinels and sulfides in platinum-group minerals are interpreted to be trapped droplets of co-existing sulfide melt. The captured sulfide melt has evolved in the direction of increasing the fugacity of sulfur: troilite + pentlandite (Fe>Ni) - in sperrylite (paragenesis I) to monoclinic pyrrhotite + pentlandite (Ni approximate to Fe) + chalcopyrite - in Pt-Fe alloys (paragenesis II). Paragenesis from the sulfide aggregates in the silicate matrix are more fractionated: pyrrhotite + pyrrhotite (Ni>Fe) + chalcopyrite (III) and pyrite + pentlandite (Ni>>Fe) + millerite (IV). Pd arsenides and antimonides crystallised later than sperrylite and isoferroplatinum, as a result of the evolution of a sulfide melt with an increased activity of the element ligands (Te, Sn, Sb and As).
- Добавил в систему: Чайка Иван Федорович
Прикрепленные файлы
| № | Имя | Описание | Имя файла | Размер | Добавлен |
|---|---|---|---|---|---|
| 1. | Полный текст | Tolstykh_et_al._2019.pdf | 1,3 МБ | 22 декабря 2020 [IvanChayka] |