The first identification of cronstedtite in Cu–Ni–PGE ores of the Talnakh intrusion; Scientific Reports; Vol. 13

The first identification of cronstedtite in Cu–Ni–PGE ores of the Talnakh intrusion; Scientific Reports; Vol. 13

Detalhes bibliográficos
Parent link:Scientific Reports.— .— New York: Springer Nature
Vol. 13.— 2023.— Article number 22437, P. 1-9
Autor Corporativo: Томский политехнический университет
Outros Autores: Yakich T. Yu. Tamara Yurievna, Zhimuleva E. S., Rudmin M. A. Maksim Andreevich, Ruban A. S. Aleksey Sergeevich, Maksimov P. N. Prokopy Nikolaevich, Shaldybin M. V. Mikhail Viktorovich
Resumo:We present new mineralogical data of cronstedtite from the Southern-2 orebody, located in the South-Western branch of the Talnakh intrusion (Noril’sk area) composed of massive sulfides in which the total amount of oxides and silicates does not exceed 1–3 vol%. The petrographic and mineralogical features of these ores indicated occurrence of fine-grained, fibrous needle like clusters < 50-µm-sized grains of cronstedtite (7.09 Å along its c-axis). This mineral confirmed by a number of analytical techniques (powder X-ray diffraction of balk samples, transmission electron microscopy, scanning electron microscopy, Raman and Infrared spectroscopy). Cronstedtite sporadically contains signals of Al, Ni, Ca and filling the cracks and cavities between sulfides of copper (chalcopyrite) and iron (pyrrhotite, pentlandite). In some cases, cronstedtite contains micron-sized PGM, and associates with magnetite. According the X-ray diffraction analysis of the bulk massive ores besides cronstendtite are established kaolinite, gypsum, calcite, quartz, and cristobalite. The findings of cronstedtite in Noril’sk area have never been mentioned publicly before. Its occurrence is the northernmost known locality in the world. Our results imply that the formation of cronstedtite in the Talnakh intrusion could be possible by the active participation low-temperatures fluids within the relatively near-surface (< 2 km of paleosurface) conditions of intrusion emplacement, in contrast to other deep-seated supergiant Cu–Ni–PGE deposits in the world. The conditions of formation in isolated cavities in fresh pyrrhotite-pentlandite-chalcopyrite massive ores of deep level of the Talnakh intrusion could be favorable for the formation of cronstendtite.
Текстовый файл
Idioma:inglês
Publicado em: 2023
Assuntos:
cronstedtite
Cu–Ni–PGE ores
Talnakh intrusion
Noril’sk sulfde
труды учёных ТПУ
электронный ресурс
Acesso em linha:https://doi.org/10.1038/s41598-023-49953-x
Formato: Recurso Electrónico Capítulo de Livro
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=671205

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