Okulitch, A. V., Cameron, B. E. B. (1976) Stratigraphic revisions of the Nicola, Cache Creek, and Mount Ida Groups, based on conodont collections from the western margin of the Shuswap Metamorphic Complex, south-central British Columbia. Canadian Journal of Earth Sciences, 13 (1) 44-53 doi:10.1139/e76-004
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | Stratigraphic revisions of the Nicola, Cache Creek, and Mount Ida Groups, based on conodont collections from the western margin of the Shuswap Metamorphic Complex, south-central British Columbia | ||
| Journal | Canadian Journal of Earth Sciences | ||
| Authors | Okulitch, A. V. | Author | |
| Cameron, B. E. B. | Author | ||
| Year | 1976 (January 1) | Volume | 13 |
| Issue | 1 | ||
| Publisher | Canadian Science Publishing | ||
| DOI | doi:10.1139/e76-004Search in ResearchGate | ||
| Generate Citation Formats | |||
| Mindat Ref. ID | 474641 | Long-form Identifier | mindat:1:5:474641:0 |
| GUID | 0 | ||
| Full Reference | Okulitch, A. V., Cameron, B. E. B. (1976) Stratigraphic revisions of the Nicola, Cache Creek, and Mount Ida Groups, based on conodont collections from the western margin of the Shuswap Metamorphic Complex, south-central British Columbia. Canadian Journal of Earth Sciences, 13 (1) 44-53 doi:10.1139/e76-004 | ||
| Plain Text | Okulitch, A. V., Cameron, B. E. B. (1976) Stratigraphic revisions of the Nicola, Cache Creek, and Mount Ida Groups, based on conodont collections from the western margin of the Shuswap Metamorphic Complex, south-central British Columbia. Canadian Journal of Earth Sciences, 13 (1) 44-53 doi:10.1139/e76-004 | ||
| In | (1976, January) Canadian Journal of Earth Sciences Vol. 13 (1) Canadian Science Publishing | ||
| Abstract/Notes | Conodonts have been recovered from highly deformed limestone and calcareous argillite in Palaeozoic and Mesozoic successions near the western border of the Shuswap Metamorphic Complex. Presently known biostratigraphic sequences indicate that the Eagle Bay Formation of the Mount Ida Group is in part Mississippian in age, and likely correlative with the Slide Mountain and Milford Groups. In addition, part of the succession previously mapped as Cache Creek Group in the Vernon area is now known to be Late Triassic in age, and can be correlated with the Sicamous Formation of the Mount Ida Group, the Nicola Group, and the Slocan Group. The Upper Triassic succession was affected by deformation and metamorphism associated with development of the Shuswap Metamorphic Complex. | ||
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