Formation of orogenic gold deposits by progressive movement of a fault-fracture mesh through the upper crustal brittle-ductile transition zone

Orogenic gold deposits are comprised of complex quartz vein arrays that form as a result of fluid flow along transcrustal fault zones in active orogenic belts. Mineral precipitation in these deposits occurs under variable pressure conditions, but a mechanism explaining how the pressure regimes evolv...

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Detalles Bibliográficos
Autores principales: Tavares Nassif, Miguel, Monecke, Thomas, Reynolds, T. James, Kuiper, Yvette D., Goldfarb, Richard J., Piazolo, Sandra, Lowers, Heather A.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2022
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9576763/
https://www.ncbi.nlm.nih.gov/pubmed/36253461
http://dx.doi.org/10.1038/s41598-022-22393-9

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9576763/
https://www.ncbi.nlm.nih.gov/pubmed/36253461
http://dx.doi.org/10.1038/s41598-022-22393-9

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