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TitleCurrent research, part D, eastern Canada and national and general programs / Recherches En Cours, Partie D, Est du Canada et Programmes Nationaux et Généraux
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AuthorGeological Survey of Canada
SourceGeological Survey of Canada, Paper no. 92-1D, 1992, 275 pages, https://doi.org/10.4095/132872 (Open Access)
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Year1992
Documentserial
Lang.English; French
Mediapaper; on-line; digital
RelatedThis publication contains the following publications
File formatpdf
ProvinceNova Scotia; New Brunswick; Quebec; Northern offshore region; Eastern offshore region; Saskatchewan; Alberta; Yukon; Manitoba; Ontario; Northwest Territories; Nunavut; Newfoundland and Labrador
NTS1K; 1L; 1M; 1N; 2C; 2D; 2E; 2L; 10M; 11C; 11D; 11F; 11G; 11J; 11K; 11O; 12A; 12H; 12I; 12P; 20P; 21E; 21G; 21H; 21L; 21O; 21P; 22A; 31H; 31I; 38C; 41I; 48B; 63M; 63N; 63O; 63P; 73O; 73P; 74H; 97C
AreaSpringdale Peninsula; Buchans; Cape Breton Island; Carmanville; Saint John; Flemish Cap; Grand Banks; Blanc-sablon; Big Bald Mountain; Serpentine Lake; Upsalquitch Forks; Port Aux Basques; Trois-rivieres; Halifax Harbour; Arctic; North Atlantic Oceans; Baie Verte Peninsula; Gaspesie; Belledune-elmtree Inlier; Pilley's Island; Canada; Ussr; Zambia
Lat/Long WENS-180.0000 180.0000 90.0000 -20.0000
Subjectseconomic geology; geochemistry; paleontology; sedimentology; stratigraphy; tectonics; geophysics; igneous and metamorphic petrology; surficial geology/geomorphology; structural geology; environmental geology; plutonic rocks; volcanic rocks; igneous rocks; metamorphic rocks; sedimentary rocks; stratigraphic correlations; alteration; radiometric dates; depositional environment; lithology; analyses; geochemical analyses; structural features; tectonic elements; tectonostratigraphic zones; landforms; deformation; metamorphism; facies; mineral deposits; sulphides; mineralization; glaciation; glacial deposits; geophysical surveys; isotopes; analytical methods; statistical methods; statistical analysis; drillholes; Acadian Orogeny; Exploits Subzone; Port Aux Basques Complex; Cape Ray Fault Zone; Stoger Tight Showing; Deschambault Formation; Gaspe Limestones; Miramichi Group; Tetagouche Group; Fournier Group; Cenozoic; Mesozoic; Paleozoic; Precambrian; Proterozoic
Illustrationstables; photomicrographs; seismic profiles; stratigraphic columns; cross-sections; photographs; sketch maps; analyses; stereonets; plots; graphs
Released1992 02 01; 2014 11 13
AbstractThe Rendell-Jackman gold deposit is one of the most significant mesothermal vein-type gold deposits in the Canadian Appalachians. It is located within a deformed Ordovician metavolcanic dominated sequence containing felsic dykes. The first episode of deformation is evidenced in the metavolcanics by an S 1 planar fabric containing a down dip stretching lineation. The second episode (Di) produced steeply plunging E-W folds, an S2 foliation and discrete brittle-ductile D2 high strain zones, affecting the metavolcanics and the felsic dykes. The se brittle-ductile D2 high strain zones are particularly well developed in the hinges of F 2Jolds. They are also strongly controlled by the layer anisotropy induced by the felsic dykes which are competent compared to the incompetent metavolcanics. The gold bearing quartz veins are of shear vein type and hosted within and sub-parallel to the D2 high strain zones. The fast deformation episode produced F3 sub-horizontal folds and Late NE and ENE brittle faults.
GEOSCAN ID132872