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Skip to Search Results- 1Dr. Larry Heaman (Earth and Atmospheric Sciences)
- 1Herd, Christopher (Earth and Atmospheric Sciences)
- 1Larry Heaman (Earth and Atmospheric Science)
- 1Pearson, Graham (Department of Earth and Atmospheric Sciences)
- 1Richards, Jeremy ( Department of Earth and Atmospheric Science)
- 1Sarah Gleeson (Department of Earth and Atmospheric Sciences)
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Age, geochemistry, and fluid characteristics of the MAX porphyry Mo deposit, southeast British Columbia
DownloadFall 2009
Lawley, Christopher John Michael
MAX is a porphyry Mo deposit located near Trout Lake village in southeastern British Columbia. Mo mineralization is hosted by variably-altered calc-alkaline granodiorite dikes. Quartz veins have been subdivided into a paragenetic sequence based on vein style and crosscutting relationships....
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Spring 2020
The timing of a diamondiferous kimberlite cluster within the Archean Superior Province, the Renard cluster (Otish field, Québec), was investigated by ID-TIMS U-Pb dating of groundmass perovskite. Few Otish field kimberlites were previously dated by U-Pb perovskite (Renard 1-3 and Lac Beaver) but...
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Dating Magmatism on Mars: Application of In-Situ and Microsampling Techniques for Shergottite Geochronology
DownloadFall 2022
Establishing an absolute time scale of Mars is critical to understanding the planet’s geological evolution. Currently, martian meteorites are the only samples of the planet available for radiometric geochronology analysis in terrestrial laboratory settings. The record of known martian absolute...
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Genesis and controls on mineralization at the Hammer Zone silver showing, Mount Mye Trend, hosted by the Anvil Batholith, South-Central Yukon
DownloadFall 2017
When Silver Range resources acquired the Keg property in 2010, one of the prospects included was the Hammer Zone. Ensuing mapping and surface sampling found the Hammer Zone to be a small, bonanza-grade, epithermal silver system contained entirely within the Anvil Batholith. Initial petrographic...
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Fall 2014
A multi-technique geochemical study of the Scourie dykes in the Lewisian gneiss complex (LGC) of northwest Scotland is presented. The Scourie dykes are a set of northwest-southeast trending mafic and ultramafic dykes that intrude the LGC between two periods of high-grade regional metamorphism....
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U-Pb geochronology and REE geochemistry of the pulsed Cretaceous magmatism in High Arctic Canada: implications for lithospheric evolution and magma genesis
DownloadFall 2016
Cretaceous magmatism in the Sverdrup Basin of Arctic Canada consists of alkalic and tholeiitic phases that are widely considered to be part of the circum-Arctic High Arctic large igneous province (HALIP). The emplacement of large igneous provinces is commonly attributed to mantle plumes. However,...