Upper Triassic to Lower Jurassic stratigraphy of the Faro Peak formation, southern Tay River map area, central Yukon (NTS 105K)
The lower and upper members of the Faro Peak formation comprise Upper Triassic and Lower Jurassic successions, respectively, that are assigned to the Yukon-Tanana terrane in the southern Tay River map area (NTS 105K). The lower member is ~650 m-thick and contains a basal conglomerate overlain by argillite, limestone, basalt, and lithic feldspathic wacke to arenite that represents part of an overlap assemblage and regionally covers Paleozoic rocks of the Yukon-Tanana terrane, Slide Mountain terrane, and ancestral Cordilleran margin. The upper member has >800 m of massive conglomerate and sandstone that overlies different stratigraphic levels of the lower member and locally sits on Yukon-Tanana basement. The upper member is coeval with Whitehorse trough strata of central Yukon and similarly records Early Jurassic exhumation of the northern Intermontane terranes. The two members are lithologically distinct, of mappable extent, and have unconformable contacts, and therefore should be separated into two new formations.
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Additional Info
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| Last Updated | October 20, 2025, 02:22 (UTC) |
| Created | October 20, 2025, 02:22 (UTC) |
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Domain / Topic
Domain or topic of the dataset being cataloged.
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Title
Title for the Dataset.
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Upper Triassic to Lower Jurassic stratigraphy of the Faro Peak formation, southern Tay River map area, central Yukon (NTS 105K) |
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Description
A description of the dataset.
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The lower and upper members of the Faro Peak formation comprise Upper Triassic and Lower Jurassic successions, respectively, that are assigned to the Yukon-Tanana terrane in the southern Tay River map area (NTS 105K). The lower member is ~650 m-thick and contains a basal conglomerate overlain by argillite, limestone, basalt, and lithic feldspathic wacke to arenite that represents part of an overlap assemblage and regionally covers Paleozoic rocks of the Yukon-Tanana terrane, Slide Mountain terrane, and ancestral Cordilleran margin. The upper member has >800 m of massive conglomerate and sandstone that overlies different stratigraphic levels of the lower member and locally sits on Yukon-Tanana basement. The upper member is coeval with Whitehorse trough strata of central Yukon and similarly records Early Jurassic exhumation of the northern Intermontane terranes. The two members are lithologically distinct, of mappable extent, and have unconformable contacts, and therefore should be separated into two new formations. |
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Metadata Identifier
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Published Date
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2020-01-16 |
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Time Period Data Span (end date)
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Access category
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License
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Open Government Licence - Yukon |
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Location
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https://open.canada.ca/data/en/dataset/47f5e84b-d083-4639-818e-4d5f97d2d302 |
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Data Service
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Owner
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Government of Yukon | Gouvernement du Yukon |
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Contact Point
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Yukon Geological Survey |
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Publisher
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Publisher Email
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[email protected] |
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Contains data about individuals
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Contains Indigenous Data
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Portal Type
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Version
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None |
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Source
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None |
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Indigenous Community Permission
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Community Permission
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