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Skip to Search Results- 1Beaton, Neil I.
- 1Hnatyshin, Danny
- 1Jones, Gabrielle
- 1Kraft, Jamie L
- 1Lacombe, Ryan A
- 1Langlois, Lauren A
- 1Banks, Jonathan (Earth and Atmospheric Science)
- 1Banks, Jonathan (Earth and Atmospheric Sciences)
- 1Creaser, Robert (Department of Earth and Atmospheric Sciences)
- 1Dr. John Waldron, EAS
- 1Dr. Philippe Erdmer, Earth and Atmospheric Sciences
- 1Erdmer, Philippe (Earth and Atmospheric Sciences)
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Stratigraphy, paleogeography and tectonic evolution of early Paleozoic to Triassic pericratonic strata in the northern Kootenay Arc, southeastern Canadian Cordillera, British Columbia
DownloadSpring 2013
The northern Kootenay Arc in southeastern British Columbia hosts a near-continuous succession of Cambrian to Permian strata that were deposited in overlapping marginal basins outboard of the Canadian Cordilleran miogeocline. The basinal strata of the Late Cambrian and younger Lardeau Group are...
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Stratigraphic and Structural Relationships in the Foreland Basin and Humber Arm Allochthon on Port au Port Peninsula, western Newfoundland
DownloadFall 2017
Port au Port Peninsula, in western Newfoundland, sits at the western edge of the Appalachian orogen. Middle Ordovician foreland basin strata deposited on the Laurentian margin are primarily derived from, and overridden by, Cambrian to Ordovician deep-water rocks previously mapped as mélange and...
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Spring 2021
The Upper Devonian Duvernay Formation is an important hydrocarbon source rock in the Western Canada Sedimentary Basin and has been a significant unconventional oil, gas liquids, and gas reservoir since 2011. Heterogeneity in this and other shale reservoirs is important in predicting rock...
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Metamorphic devolatilization, mineral reaction, and fluid alteration in the Mica Creek area (British Columbia, Canada) inferred from whole-rock and mineral nitrogen isotope signatures
DownloadSpring 2019
The Neoproterozoic Horsethief Creek Group metasedimentary rocks in the Mica Creek area (British Columbia, Canada) are an important supracrustal sequence in the Canadian Cordillera. They contain a continuous range of metamorphic grades from slate, progressively to schists in the biotite, garnet,...
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Indicators of gold mineralization in the Yellowknife greenstone belt: a lithogeochemistry and mineralogy study
DownloadSpring 2021
Geochemical signatures within an economic deposit are an important indicator used in the exploration of high-grade mineralization. In this study, we aim to identify elements that can act as geochemical indicators for orogenic gold within the Yellowknife greenstone belt that allow the...
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Implications of in situ zircon U-Pb, Lu-Hf, oxygen-isotope, and trace element geochemistry on the petrogenetic history of the northern Hogem batholith in the Quesnel terrane, north-central British Columbia, Canadian Cordillera
DownloadSpring 2022
The Cordilleran orogen of western Canada is a type example of accretionary tectonism and thus an ideal location to study continental growth by oceanic and continental arc magmatism and terrane accretion. Cordilleran Intermontane terranes are interpreted as accreted oceanic arcs that contributed...
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Fall 2017
The Bakken Formation is the most productive formation in the Williston Basin and one of the most important tight oil plays in North America. Oil in the Bakken Formation has been shown to migrate from the mature, central portion of the Williston Basin outwards towards the less mature portions of...
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Geothermal Reservoir Characterization of the South Swan Hills Oil Pool, Swan Hills, Alberta
DownloadSpring 2022
Research in the South Swan Hills oil pool was performed to accurately delineate the geometry of the subsurface reservoir and subsequently quantify the amount of thermal energy that can be extracted for geothermal use from the reservoir water volume. South Swan Hills is an active oilfield...
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Geology, Geochemistry, Geochronology, and economic potential of the Taftan volcanic complex, southeastern Iran
DownloadFall 2015
Razavi Khosroshahi, Seyed Amir Mohammad
The late Miocene-Quaternary Taftan volcanic complex is located above the Makran subduction zone in Sistan and Baluchestan province of southeastern Iran. The earliest volcanic eruptions at Taftan started in the late Miocene (~8 Ma) by explosive eruption of andesitic to dacitic lava on the...
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Geology of the Nicola Group in the vicinity of the Iron Mask batholith, Kamloops, British Columbia
DownloadSpring 2010
Two regional scale deformation events are observed in the Kamloops region. A Late Triassic-Early Jurassic southwest directed compressional event and a later Tertiary extensional deformation episode, manifested in the uplift of the Nicola horst. The Nicola horst is bounded to the northeast by the...