| Titre | Chemical fingerprinting of the Archean Côté Gold deposit: a large-tonnage, low-grade intrusion-related deposit system, Ontario, Canada |
| Télécharger | Téléchargement (publication entière) |
| Auteur | Katz, L R; Kontak, D J; Dubé, B; Rogers, J R |
| Source | TGI 4 - Intrusion Related Mineralisation Project: new vectors to buried porphyry-style mineralisation; par Rogers, N (éd.); Commission géologique du Canada, Dossier public 7843, 2015 p. 445-458, https://doi.org/10.4095/296482 (Accès ouvert) |
| Liens | Canadian Database of Geochemical Surveys, downloadable files
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| Liens | Banque de données de levés géochimiques du Canada,
fichiers téléchargeables
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| Année | 2015 |
| Éditeur | Ressources naturelles Canada |
| Document | dossier public |
| Lang. | anglais |
| DOI | https://doi.org/10.4095/296482 |
| Media | en ligne; numérique |
| Référence reliée | Cette publication est contenue dans Rogers, N;
(2015). TGI 4 - Intrusion Related Mineralisation Project: new vectors to buried porphyry-style mineralisation, Commission géologique du Canada, Dossier public 7843 |
| Formats | pdf |
| Province | Ontario |
| SNRC | 32D/01; 32D/02; 32D/07; 32D/08 |
| Lat/Long OENS | -78.6000 -78.4000 48.2833 48.2167 |
| Sujets | gisements porphyriques; cuivre porphyrique; prospection minière; minéralisation; or; altération; tungstène; molybdène; étain; bismuth; gisements minéraux; roches intrusives; roches granitiques; gîtes
magmatiques; altération hydrothermale; roches ignées; gisements minéraux hydrothermaux; Archéen; géologie économique; géochimie; Précambrien |
| Illustrations | location maps; photographs; photomicrographs; plots |
| Consultation | |
| Bibliothèque de Ressources naturelles Canada - Ottawa (Sciences de la Terre) |
| |
| Programme | Étude des gîtes porphyriques, Initiative géoscientifique ciblée (IGC-4) |
| Diffusé | 2015 06 11 |
| Résumé | (disponible en anglais seulement)
The Côté Gold intrusion-related Au (-Cu) deposit, in the Archean Swayze greenstone belt of the Abitibi Subprovince, is a large-tonnage, low-grade deposit hosted
by ca. 2741 Ma tonalite and diorite of the Chester intrusive complex which formed in a high-level sub-volcanic setting. The deposit contains a resource (indicated + inferred) of 8.3 M oz Au that is centered on a magmatic-hydrothermal breccia.
Mineralisation occurs as disseminations or is associated with quartz ± carbonate vein arrays, and is broadly coincident with biotite, silica-sodic and sericite alteration zones. Lithogeochemical and petrographic/SEM-EDS studies (>600 samples) across
the deposit are used to assess the petrogenesis of the magmatic host rocks, distinguish between magmatic versus hydrothermal breccia, differentiate alteration types, determine the precursor rock where alteration is most intense, and chemically
fingerprint the deposit. Preliminary observations indicate the following: (1) the tonalite suite is characterised by unfractionated CN REE patterns and reflects melt generation in a low-P regime; (2) protolith rocks are best discriminated using CaO,
TiO2 and Zr/TiO2; (3) the magmatic-hydrothermal breccia is characterised by an Au-Cu-F-Te-Zn association; (4) biotite alteration, often with intergrowth of chalcopyrite, is characterised by Ba and LREE enrichment often accompanied by the presence of
allanite-euxenite-bastnaesite; (5) zones of intense sodic alteration, up to 40 m thick and approaching 10 wt% Na2O are characterised by a red-pink colour and a vuggy texture due to quartz dissolution. In thin section albite is pitted, contains
abundant fluid inclusions and is mantled by clear albite. These rocks are considered to be episyenites; (6) sericite alteration zones, up to 150 m and cutting silica-sodic alteration, are characterised by an F ± Au ± Cu association; and (7) the
chemistry of biotite in the breccia unit shows a reversal in Mg# after fractionation from diorite to tonalite (i.e., decreasing Mg#) which may indicate either injection of a new primitive melt or an oxidation-sensitive event coincident with formation
of the breccia. Many of the features of the Côté Gold deposit suggest derivation of mineralisation and alteration by the flux of high-temperature fluids enriched in K, Fe, F, LREE, CO2, and Ba, in addition to Au, Te and Cu. The association of Au-Cu
mineralisation with a magmatic-hydrothermal breccia and a chemical signature that is atypical for Archean orogenic-type gold deposits indicates a possible affinity with a spatially and temporally related intrusive centre. |
| GEOSCAN ID | 296482 |
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