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Grant: Discovery Grants Program - Individual

University of Toronto

$1,354.00

Advancements in U-Pb dating of deep crustal structures and magmatic/meteoritic events in relation to biotic evolution in earth history

EF 2009-10

Résumé
Precise uranium-lead analyses of minute (microgram) quantities of the mineral 'zircon' that crystallize during formation, reheating, or ductile flow events provide detailed scenarios of the evolution of the Earth's crust during periods of mountain building. When enormous continental plates collide, this produces over-thickened stacks of crustal rocks such that the lower part of the thrust stack is heated from below and softened and slides further inland. This must have happened under the Rocky Mountains as this thick pile of sedimentary material, once at the ocean bottom, now sits above an older continent. To understand processes that took place along the interface, 10 - 20 km below the Earth's surface where we cannot see, we must find a very old mountain root where the mountains have since been removed by erosion. The Grenville Province, well exposed along Georgian Bay, Ontario, is such a root. Here, geologists who study the rock record observe both the old, cold solid lower plate and the soft, hot overlying rocks that moved overtop during a great plate collision more than a billion years ago. In short, we discover the nature of the processes that put the Rockies in their place. The evolution of life on Earth has been subject to sudden drastic losses of species over brief time intervals that are recorded in the rock record. These mass extinction events can be correlated with meteorite impacts and major volcanic eruptions. Using high resolution U-Pb dating methods we can accurately pinpoint the time of these meteoritic/volcanic events and establish or refute synchronicity with the extinction events by dating volcanic ash beds that occur near the extinction horizons. My research also involves new strategies in the field to select rocks in complex gneiss terranes that give age information directly tied to once active tectonic processes. I am also developing methods in the laboratory to better resolve complex, multi-stage, zircon populations that occur in metamorphic rocks, and to make U-Pb ages more precise.
Programme
Discovery Grants Program - Individual
Bénéficiaire
Emplacement
Ontario, Canada
Type de bénéficiaire
Academia
Type
Grant
Source
NSERC's Awards Data

Tel que publié

Application id
4261-2007
Name nom
Krogh, Thomas
Department département
Geology
Organization id
31
Institution établissement
University of Toronto
Province en
Ontario
Province fr
Ontario
Country en
CANADA
Country fr
CANADA
Fiscal year exercice financier
2009
Competition year année de concours
2007
Award amount
1354
Program id
RGPIN
Program nane en
Discovery Grants Program - Individual
Program name fr
Programme de subventions à la découverte - individuelles
Group en
Discovery grants programs
Group fr
Programmes de subventions à la découverte
Committee code
8
Committee name en
Solid Earth Sciences
Committee name fr
Sciences de la Terre solide
Area of application code
1203
Area of application group en
Advancement of knowledge
Area of application group fr
Avancement des connaissances
Area of application en
Earth sciences
Area of application fr
Sciences de la terre
Research subject code
4204
Research subject group en
Geochemistry and geochronology
Research subject group fr
Géochimie et géochronologie
Research subject en
Geochronology
Research subject fr
Géochronologie
Partie
3
Nb partie
3
Application title
Advancements in U-Pb dating of deep crustal structures and magmatic/meteoritic events in relation to biotic evolution in earth history
Keyword
NA
Application summary
Precise uranium-lead analyses of minute (microgram) quantities of the mineral 'zircon' that crystallize during formation, reheating, or ductile flow events provide detailed scenarios of the evolution of the Earth's crust during periods of mountain building. When enormous continental plates collide, this produces over-thickened stacks of crustal rocks such that the lower part of the thrust stack is heated from below and softened and slides further inland. This must have happened under the Rocky Mountains as this thick pile of sedimentary material, once at the ocean bottom, now sits above an older continent. To understand processes that took place along the interface, 10 - 20 km below the Earth's surface where we cannot see, we must find a very old mountain root where the mountains have since been removed by erosion. The Grenville Province, well exposed along Georgian Bay, Ontario, is such a root. Here, geologists who study the rock record observe both the old, cold solid lower plate and the soft, hot overlying rocks that moved overtop during a great plate collision more than a billion years ago. In short, we discover the nature of the processes that put the Rockies in their place. The evolution of life on Earth has been subject to sudden drastic losses of species over brief time intervals that are recorded in the rock record. These mass extinction events can be correlated with meteorite impacts and major volcanic eruptions. Using high resolution U-Pb dating methods we can accurately pinpoint the time of these meteoritic/volcanic events and establish or refute synchronicity with the extinction events by dating volcanic ash beds that occur near the extinction horizons. My research also involves new strategies in the field to select rocks in complex gneiss terranes that give age information directly tied to once active tectonic processes. I am also developing methods in the laboratory to better resolve complex, multi-stage, zircon populations that occur in metamorphic rocks, and to make U-Pb ages more precise.