{"database":"biostudies-literature","file_versions":[],"scores":null,"additional":{"omics_type":["Unknown"],"volume":["17(1)"],"submitter":["Demmer M"],"pubmed_abstract":["The synchronous formation between 2675-2655 Ma of hydrothermal gold mineralisation in the Kalgoorlie and Kurnalpi Terranes and of magmatic sulfide mineralisation enriched in nickel, copper and platinum-group elements in the South West Terrane of the Archean Yilgarn Craton of Western Australia offers key insights into first-order controls on the genesis of mineral systems. Here we show that hydrothermal and magmatic deposits formed on opposite sides of this craton share four key features: timing, enrichment in incompatible chalcophile elements, positive Δ³³S sulfur isotope signatures, and links to hydrous, metasomatised lithospheric mantle. These commonalities challenge conventional models that treat such mineralised systems as unrelated. Instead, they point to a shared origin: a fertile li"],"journal":["Nature communications"],"pagination":["1798"],"full_dataset_link":["https://www.ebi.ac.uk/biostudies/studies/S-EPMC12917142"],"repository":["biostudies-literature"],"pubmed_title":["Unveiling the metallogenic continuum of an Archean craton."],"pmcid":["PMC12917142"],"pubmed_authors":["Ezad I","Demmer M","Fiorentini M"],"additional_accession":[]},"is_claimable":false,"name":"Unveiling the metallogenic continuum of an Archean craton.","description":"The synchronous formation between 2675-2655 Ma of hydrothermal gold mineralisation in the Kalgoorlie and Kurnalpi Terranes and of magmatic sulfide mineralisation enriched in nickel, copper and platinum-group elements in the South West Terrane of the Archean Yilgarn Craton of Western Australia offers key insights into first-order controls on the genesis of mineral systems. Here we show that hydrothermal and magmatic deposits formed on opposite sides of this craton share four key features: timing, enrichment in incompatible chalcophile elements, positive Δ³³S sulfur isotope signatures, and links to hydrous, metasomatised lithospheric mantle. These commonalities challenge conventional models that treat such mineralised systems as unrelated. Instead, they point to a shared origin: a fertile li","dates":{"release":"2026-01-01T00:00:00Z","publication":"2026 Jan","modification":"2026-07-16T10:03:16.913Z","creation":"2026-07-09T10:48:20.126Z"},"accession":"S-EPMC12917142","cross_references":{"pubmed":["41545390"],"doi":["10.1038/s41467-026-68507-z"]}}