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TitleNew U-Pb dates from southwestern Coast Belt, British Columbia
DownloadDownload (whole publication)
AuthorMonger, J W H; McNicoll, V J
SourceRadiogenic age and isotopic studies: report 7; by Geological Survey of Canada; Geological Survey of Canada, Paper no. 93-2, 1993 p. 119-126, https://doi.org/10.4095/193341
Year1993
PublisherNatural Resources Canada
Documentserial
Lang.English
Mediapaper
RelatedThis publication is contained in Geological Survey of Canada; (1993). Radiogenic age and isotopic studies: report 7, Geological Survey of Canada, Paper no. 93-2
ProvinceBritish Columbia
NTS92G/NW; 92K
AreaQuadra Island; Bute Inlet; Howe Sound
Lat/Long WENS-126.0000 -123.0000 51.0000 49.5000
Subjectsgeochronology; granites; igneous rocks; zircon dates; uranium lead dates; radiometric dates; Mount Roderick Granodiorite; Ward Point Pluton; Paradise River Pluton; Bodega Point Pluton; Coast Belt; Insular Belt; Jurassic; Cretaceous
Illustrationssketch maps; analyses; Concordia diagrams
Released1994 01 01
AbstractFour new U-Pb dates of granitic rocks from the southwestern Coast Belt are reported. The Bodega Point pluton on Quadra Island, Bute Inlet map-area (92K), is the westernmost Coast Belt pluton at this latitude and intrudes Wrangellian stratigraphy; it has been dated at 163.8 +/- 0.4 Ma, Middle Jurassic. To the northeast, along Bute Inlet, two samples were analyzed from a region of granitic rocks previously mapped as mostly of Cretaceous age. The Paradise River pluton, at 145 +/- 2 Ma, is latest Jurassic, similar in age to the Cloudburst quartz diorite in Vancouver map area (92G). The Ward Point pluton is 153.6 +/- 0.4 Ma, Late Jurassic; this age is comparable to others in southwestern Coast Belt. Granodiorite on Mount Roderick, apparently part of a regionally extensive composite body herein called the Howe Sound batholith, yields a mid-Cretaceous age of 95.8 +/- 1 Ma. This date places a maximum age on contractional deformation on the Britannia shear zone near Howe Sound, and falls within the period spanned by regional deformation in the southeastern Coast Belt.
GEOSCAN ID193341