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TitreStructural and diagenetic origin of breccias in the carbonate-hosted Polaris Zn-Pb deposit, Nunavut, Canada
AuteurReid, S; Dewing, K; Sharp, R
SourceOre Geology Reviews vol. 55, 2013 p. 110-124, https://doi.org/10.1016/j.oregeorev.2013.05.003
Année2013
Séries alt.Secteur des sciences de la Terre, Contribution externe 20120354
ÉditeurElsevier
Documentpublication en série
Lang.anglais
DOIhttps://doi.org/10.1016/j.oregeorev.2013.05.003
Mediapapier; en ligne; numérique
Formatspdf
ProvinceNunavut
SNRC58B; 58C; 58F; 58G; 59B; 59C; 68A; 68D; 68E; 68H; 69A; 69D
Lat/Long OENS-100.0000 -92.0000 77.5000 72.0000
Sujetsgisements minéraux; gîtes minéralogiques; zinc; plomb; minéralisation; roches carbonatées; carbonates; gîtes de la vallée du mississippi; gisements minéraux hydrothermaux; altération hydrothermale; roches sédimentaires; dolomites; brèches; Mine Polaris ; géologie économique; géologie structurale; stratigraphie; Paléozoïque; Ordovicien
Illustrationslocation maps; stratigraphic columns; cross-sections; photographs
ProgrammeBassin sédimentaire Sverdrup, GEM : La géocartographie de l'énergie et des minéraux
Résumé(disponible en anglais seulement)
The Polaris deposit, located on Little Cornwallis Island in the Canadian Arctic, was a Mississippi Valley-type Zn - Pb deposit hosted by brecciated carbonate rocks of the Upper Ordovician Thumb Mountain Formation. Mapping indicates that strike-slip faults on the east side of the Polaris deposit were active during the last stage of the Late Devonian Ellesmerian Orogeny. Polaris is on a jog in the north-oriented, Early Devonian Boothia fault system and was the site of localized extension during south-directed Late Devonian Ellesmerian compression. This structural setting elsewhere in the district may be prospective for Zn - Pb mineralisation.
Ore fluids rising in the Late Devonian interacted with the host rock causing dissolution, brecciation and collapse. Carbonate beds are thinned, indicating widespread removal of carbonate material. Five breccia types (crackle, pseudo, cobble, mega and collapse) are present in the vicinity of the deposit. Crackle breccia is preserved around the periphery of the deposit and is indicative of structural dilation or the early stages of mineralisation. Dolomite and pseudobreccias are also preserved around, and extend beyond, the periphery of the deposit. These are considered an early stage of alteration directly related to the mineralising fluids and could act as a vector to the centre of the mineralising system where collapse, mega and cobble breccias occur intimately with massive mineralisation.
GEOSCAN ID292153