Aurora
Aurora is our weekly newsletter aimed at faculty, staff, and students of the department.
Aurora is our weekly newsletter aimed at faculty, staff, and students of the department.
Geofirma Engineering Ltd. is looking to hire multiple contract geoscientist positions to join the Geofirma Team. While Geofirma operates out of our Ottawa, Ontario office, the primary duties for these positions will be to provide field support as part of geoscientific site investigation activities (South Bruce) near Teeswater, Ontario. Contract positions will run between 6 and 12 months duration starting in April 2021. During intensive field activities, work will be scheduled as 12-hour shifts (day or night) for a two-week rotation. Alternate rotations can be discussed and may be considered.
The responsibilities of the position will include, but are not limited to:
A good fit for this position will include:
To find out more, visit Geofirma's website or contact them at careers@geofirma.com
Geofirma Engineering Ltd. is looking to hire multiple contract geoscientist positions to join the Geofirma Team. While Geofirma operates out of our Ottawa, Ontario office, the primary duties for these positions will be to provide field support as part of geoscientific site investigation activities (South Bruce) near Teeswater, Ontario. Contract positions will run between 6 and 12 months duration starting in April 2021. During intensive field activities, work will be scheduled as 12-hour shifts (day or night) for a two-week rotation. Alternate rotations can be discussed and may be considered.
The responsibilities of the position will include, but are not limited to:
A good fit for this position will include:
To find out more, visit Geofirma's website or contact them at careers@geofirma.com
Geofirma Engineering Ltd. is looking to hire multiple contract geoscientist positions to join the Geofirma Team. While Geofirma operates out of our Ottawa, Ontario office, the primary duties for these positions will be to provide field support as part of geoscientific site investigation activities (South Bruce) near Teeswater, Ontario. Contract positions will run between 6 and 12 months duration starting in April 2021. During intensive field activities, work will be scheduled as 12-hour shifts (day or night) for a two-week rotation. Alternate rotations can be discussed and may be considered.
The responsibilities of the position will include, but are not limited to:
A good fit for this position will include:
To find out more, visit Geofirma's website or contact them at careers@geofirma.com
The Institut des sciences de la mer de Rimouski (ISMER) of the Université du Québec à Rimouski (UQAR), a multidisciplinary research center in oceanography, is seeking a new professor of chemical oceanography with a specialization in the development of biomarkers.
The area of expertise sought is marine chemistry with an interest in biomarkers and their development from the molecular scale to the organism, molecular or isotopic tools, the land-sea continuum and environmental and climatic changes at different temporal and spatial scales. The selected candidate will be encouraged to develop his/her own area of research, to develop and manage his/her laboratory, and collaborate with researchers at ISMER and from other departments within the university. The selected candidate will participate in the MSc, PhD and DESS (Specialized Graduate Diploma) oceanography programs through the supervision of graduate students and teaching. The working language is French.
At the time of hiring, the chosen person must have a doctorate in a relevant discipline (marine chemistry, oceanography, biogeochemistry of aquatic environments or related discipline), at least one year of postdoctoral experience and a solid publication record.
Application files must include a motivation letter, a CV including the research and student training experiences and the name and contact details of three referees. Evaluation of applications will begin on July 5, 2021, and will continue until the position is filled.
Candidates interested in this position are invited to submit their application to:
Président de l’Assemblée institutionnelle
Institut des sciences de la mer de Rimouski (ISMER)
Université du Québec à Rimouski
310, allée des Ursulines, Rimouski (Québec), G5L 3A1, CANADA
By email: presid-assemblee_ismer@uqar.ca
The Institut des sciences de la mer de Rimouski (ISMER) of the Université du Québec à Rimouski (UQAR), a multidisciplinary research center in oceanography, is seeking a new professor of biological oceanography with a specialization in phytoplankton ecology.
The selected candidate must be specialized in phytoplankton ecology. The areas of expertise sought are phytoplankton ecology, molecular tools, including omic methods, for the study of biodiversity, marine planktonic biodiversity, specific and functional diversity and marine ecology. The selected candidate will be encouraged to develop his/her own area of research, to develop and manage his/her laboratory, and collaborate with researchers at ISMER and from other departments within the university. The selected candidate will participate in the MSc, PhD and DESS (Specialized Graduate Diploma) oceanography programs through the supervision of graduate students and teaching. The working language is French.
At the time of hiring, the chosen person must have a doctorate in a relevant discipline (oceanography
(biology), marine biology or ecology, ecology, zoology or biology with a thesis in marine ecology or related discipline), at least one year of postdoctoral experience and a solid publication record.
Application files must include a motivation letter, a CV including the research and student training experiences and the name and contact details of three referees. Evaluation of applications will begin on July 5, 2021, and will continue until the position is filled.
Candidates interested in this position are invited to submit their application to:
Président de l’Assemblée institutionnelle
Institut des sciences de la mer de Rimouski (ISMER)
Université du Québec à Rimouski
310, allée des Ursulines, Rimouski (Québec), G5L 3A1, CANADA
By email: presid-assemblee_ismer@uqar.ca
Title: Monazite, zircon, garnet, and corundum growth in the Thor-Odin migmatite dome as a record of metamorphism and partial melting in the southern Canadian Cordilleras
Speaker: Lindsey Abdale, MSc student Geological Sciences
Date & Time: Thursday, March 25th at 10:00am
Place: Zoom Room!
Abstract:
Using petrological observations, mineral chemistry, and thermodynamic modeling to track and constrain melting and melt crystallization in the context of polyphase exhumation of thickened continental crust. Specific segments of P-T paths are linked with accessory mineral growth using zircon, monazite, garnet, staurolite, sillimanite, and corundum thermobarometry and modeled accessory phases as well as in situ monazite and zircon ages for different growth domains. The goal of this study is to improve our understanding of the timescales and nature of exhumation of thickened continental crust that has undergone anatexis. The results demonstrate how the integration of these data can provide critical information about the tectonic and thermal history of the Cordilleran foreland belt and the evolution of metamorphic core complexes.
Title: A Metal on the Move: Examples of Crustal Uranium Cycling in the Churchill Province, Canada
Date & Time: Thursday, March 25th at 11:00am
Place: Zoom Room!
Abstract:
Uranium is designated a “critical element” as it is essential for Canada’s economic security, used mainly as a low-carbon source of energy in nuclear power production. In 2019, Canada was ranked second globally in uranium production and the fourth major exporter, supplying 13% and exporting 12% of the world’s uranium. The largest high-grade uranium resources in the world are in Saskatchewan, occurring in unconformity-type uranium deposits near the contact of the Paleoproterozoic Athabasca Basin with crystalline basement rocks of the Churchill Province. Similar, lower grade styles of mineralization are recognized in, and below, the Paleoproterozoic Thelon, and Nonacho basins, located to the north and northwest of the Athabasca Basin in the Churchill Province.
In this colloquium, we will discuss the geochemistry and mineralogy of uranium, including its mobility during crustal reworking (e.g., partial melting, fractional crystallization, metamorphism) and fluid-rock interaction (e.g., hydrothermal alteration and weathering). We will explore examples of these processes recorded in different styles of uranium mineralization throughout the Churchill Province. Current models for the formation of unconformity-type uranium deposits will be discussed, and the different styles of uranium mineralization in the Churchill Province will be compared. Following this review, we will then evaluate potential source reservoirs that supplied uranium to the deposit styles, and the processes responsible for the formation of the world-class unconformity-type uranium deposits of the Athabasca Basin.
Title: Protracted Fluid-Rock Interaction Recorded by the P2 Fault, McArthur River Deposit, Athabasca Basin, Canada: Implications for the Controls of Unconformity-Type Uranium Deposits
Date & Time: Friday, March 26th at 11:00am
Place: Zoom Room!
Abstract:
The Athabasca Basin, northern Saskatchewan, Canada, is host to world-class unconformity-type uranium deposits – high-grade, mono- to polymetallic, pods of uraninite (+secondary uranium minerals) immediately above or below the interface between Paleoproterozoic continental sandstone/conglomerate and Archean to Paleoproterozoic, crystalline, magmatic to metasedimentary basement rock. Basement-hosted uranium mineralization of the eastern Athabasca is typically found along reactivated and graphitic basement faults, and spatially associated with impermeable units of basement “quartzite”. These deposits form by the reduction of oxidized and highly saline, uraniferous basinal fluids by either a reduced basement-sourced fluid or these graphite-rich structures. In this seminar, we will examine the paragenesis, mineral chemistry and geochronology of alteration minerals along the P2 fault, which hosts the McArthur River Deposit, the largest high-grade uranium deposit yet discovered at over 2.5 Mt grading 6.91 %U3O8. The results of this research show that the P2 fault was the site of protracted hydrothermal activity since its formation during the Trans Hudson Orogen (~1840 to 1775 Ma; U-Pb rutile). Early hydrothermal activity, promoted by regional asthenosphere upwelling from 1770 to 1730 Ma (U-Pb rutile), remobilized graphite and produced extensive silicification (“quartzite”) upon cooling (1730 to 1700 Ma; U-Pb rutile), which prepared structurally and chemically viable sites for later uranium mineralizing fluids of the basin after its deposition (<1700 Ma). The incursion of basinal fluids into the basement is clocked at 1569 ±31 Ma (U-Pb anatase), within error of the main stage of uranium deposition. Although oxidizing basinal fluids are recorded in alteration minerals along the entire fault in the basement, reducing fluids are only evident in the ore zones, suggesting the main control of ore deposition was the availability of reducing fluids in the structurally and chemical viable areas.
Please join the UBC Graduate Student Society and the UBC Faculty of Medicine (FoM) Graduate and Postdoctoral Education Office for a series of Science Communication workshops, a Twitter Research Conference, as well as a closing keynote with Dr. Jennifer Gardy from March 29 to 31st, 2021!