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TitleField mapping of the Eastern Highlands Shear Zone, Cape Breton Island, Nova Scotia
DownloadDownload (whole publication)
AuthorPiette-Lauzière, N; Larson, K P; Kellett, D A
SourceTargeted Geoscience Initiative: 2017 report of activities, volume 1; by Rogers, N (ed.); Geological Survey of Canada, Open File 8358, 2018 p. 23-29, https://doi.org/10.4095/306400 (Open Access)
Year2018
PublisherNatural Resources Canada
Documentopen file
Lang.English
Mediaon-line; digital
RelatedThis publication is contained in Rogers, N; (2018). Targeted Geoscience Initiative: 2017 report of activities, volume 1, Geological Survey of Canada, Open File 8358
File formatpdf
ProvinceNova Scotia
NTS11K/09; 11K/10
AreaCanadian Appalachians; Cape Breton Island
Lat/Long WENS -60.7492 -60.4144 46.7467 46.5644
Subjectseconomic geology; tectonics; structural geology; mineral deposits; mineral exploration; mineral potential; porphyry deposits; polymetallic ores; ore mineral genesis; ore controls; structural controls; structural features; shear zones; faults; lineations; tectonic evolution; tectonic setting; metamorphism; deformation; brecciation; hydrothermal alteration; magmatism; intrusions; emplacement; accretion; kinematic analysis; fabric analysis; trend surface analysis; bedrock geology; lithology; igneous rocks; intrusive rocks; granites; granodiorites; tonalites; diorites; volcanic rocks; rhyolites; tuffs; sedimentary rocks; greywackes; volcano-sedimentary strata; metasedimentary rocks; psammites; metamorphic rocks; marbles; amphibolites; gneisses; orthogneisses; garnet; Eastern Highlands Shear Zone; Bras-d'Or Terrane; Aspy Terrane; Ganderia; Appalachian Accretionary Belt; Avalonia; Acadian Orogeny; Roper Brook Diorite; Appalachian Orogeny; ore systems approach; geological mapping; reactivation; meta-conglomerates; Phanerozoic; Paleozoic; Devonian; Silurian
Illustrationsgeoscientific sketch maps; cross-sections; photographs; photomicrographs
ProgramKnowledge Management Coordination, Targeted Geoscience Initiative (TGI-5)
ProgramPorphyry systems, Targeted Geoscience Initiative (TGI-5)
Released2018 01 19
AbstractThe Eastern Highlands shear zone (EHSZ) is located on Cape Breton Island where it separates rocks of the Bras-d'Or and Aspy terranes within Ganderia in the Appalachian accretionary belt. It records late Silurian to Early Devonian shear with east-over-west kinematics (D1) and a second deformation event (D2) with oblique dextral and west-over-east kinematics of unknown timing. Field mapping and thin section observations identified a third deformation event (D3) with brittle ductile fabrics, brecciation and hydrothermal alteration of a granite on the Aspy side of the EHSZ. These new mapping results contribute to our understanding of the later stages of deformation and their interplay with hydrothermal alteration. They also provide the framework for further studies attempting to reconstruct the postorogenic reactivation of the EHSZ and the associated magmatic-hydrothermal processes that may have contributed to the mineral endowment of the orogen.
GEOSCAN ID306400