Grant: Discovery Grants Program - Individual
Acadia University
$22,000.00
Tectonic history of the northern Appalachian orogen
EF 2013-14
Résumé
Remnants of ancient mountain belts of various ages form most of the Earth's continents, including Canada. These remnants provide an opportunity to investigate mountain-building processes by exposing the internal architecture of the former mountains. My research proposal focuses on understanding the originally separate components (or ""terranes"") that came together between about 650 and 320 million years ago to form the Appalachian mountain belt. I hope to figure out more accurately when the pieces came together within that time span, whether they came as numerous separate blocks or as a single large composite block, and from where they came - possible source areas are now located in other continents, such as South America, Africa, and Europe, or they could have been pieces of ancestral North America that broke away and then came back again. My students and I will examine rocks in the field and map their distribution. We will collect representative samples and then in collaboration with colleagues who have the necessary equipment and expertise, we will find out the precise ages of the rocks and determine their mineral and chemical (including isotopic) compositions. We are planning to measure their ancient magnetic field directions, which can help us to estimate where they were located relative to the Earth's poles when they formed. Fossils present in the rocks will help us to know their ages relative to one another. All of these different types of information will be utilized to make interpretations about what was happening (and where) at the various times when each kind of rock was forming. Some features of the rocks, such as their isotopic compositions, may help us to know what kinds of rocks underlie those that we see at the surface, information that will help us to interpret from where the various terranes were derived. It is important to understand events and processes that happened even so long ago because they shaped the environment in which we now live, and provided the natural resources that enable us to not only survive but thrive on the Earth.
Programme
Discovery Grants Program - Individual
Bénéficiaire
Emplacement
Nova Scotia, Canada
Type de bénéficiaire
Academia
Type
Grant
Source
NSERC's Awards Data
Tel que publié
Application id
4230-2011
Name nom
Barr, Sandra
Department département
Earth and Environmental Science
Organization id
78
Institution établissement
Acadia University
Province en
Nova Scotia
Province fr
Nouvelle-Écosse
Country en
CANADA
Country fr
CANADA
Fiscal year exercice financier
2013
Competition year année de concours
2011
Award amount
22000
Program id
RGPIN
Program name 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
1506
Committee name en
Geosciences
Committee name fr
Géosciences
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
4002
Research subject group en
Earth science
Research subject group fr
Sciences de la terre
Research subject en
Petrology, igneous and metamorphic geology
Research subject fr
Pétrologie, géologie ignée et métamorphique
Partie
3
Nb partie
5
Application title
Tectonic history of the northern Appalachian orogen
Keyword
NSERC
Application summary
Remnants of ancient mountain belts of various ages form most of the Earth's continents, including Canada. These remnants provide an opportunity to investigate mountain-building processes by exposing the internal architecture of the former mountains. My research proposal focuses on understanding the originally separate components (or ""terranes"") that came together between about 650 and 320 million years ago to form the Appalachian mountain belt. I hope to figure out more accurately when the pieces came together within that time span, whether they came as numerous separate blocks or as a single large composite block, and from where they came - possible source areas are now located in other continents, such as South America, Africa, and Europe, or they could have been pieces of ancestral North America that broke away and then came back again. My students and I will examine rocks in the field and map their distribution. We will collect representative samples and then in collaboration with colleagues who have the necessary equipment and expertise, we will find out the precise ages of the rocks and determine their mineral and chemical (including isotopic) compositions. We are planning to measure their ancient magnetic field directions, which can help us to estimate where they were located relative to the Earth's poles when they formed. Fossils present in the rocks will help us to know their ages relative to one another. All of these different types of information will be utilized to make interpretations about what was happening (and where) at the various times when each kind of rock was forming. Some features of the rocks, such as their isotopic compositions, may help us to know what kinds of rocks underlie those that we see at the surface, information that will help us to interpret from where the various terranes were derived. It is important to understand events and processes that happened even so long ago because they shaped the environment in which we now live, and provided the natural resources that enable us to not only survive but thrive on the Earth.