Characterizing the supra- and subsolidus processes that generated the Current PGE–Cu–Ni deposit, Thunder Bay North Intrusive Complex, Canada: insights from trace elements and multiple S isotopes of sulfides

The Current deposit is hosted by serpentinized peridotite that intruded rocks of the Quetico Subprovince in the Midcontinent Rift, and is subdivided into three morphologically distinct regions — the shallow and thin Current–Bridge Zone in the northwest, the deep and thick 437–Southeast Anomaly (SEA)...

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Detalles Bibliográficos
Autores principales: Brzozowski, M., Hollings, P., Heggie, G., MacTavish, A., Wilton, D., Evans-Lamswood, D.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Springer Berlin Heidelberg 2023
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10598094/
https://www.ncbi.nlm.nih.gov/pubmed/37885758
http://dx.doi.org/10.1007/s00126-023-01193-9

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10598094/
https://www.ncbi.nlm.nih.gov/pubmed/37885758
http://dx.doi.org/10.1007/s00126-023-01193-9

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