Grant: Discovery Grants Program - Individual
Acadia University
$50,200.00
Terrane provenance and evolution in the northern appalachian orogen
FY 2006-07
Summary
Remnants of ancient mountain belts 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. This proposal focuses on understanding the separate distinct components (or "terranes") that came together to form the part of the Appalachian mountain belt in southern New Brunswick and Nova Scotia between about 650 and 350 million years ago. I want to figure out more exactly when the pieces came together, whether they came as numerous separate blocks or as a single composite block, and from where they came - possible source areas are any of the other continents, such as South America, Africa, and Scandinavia. Although each mountain belt on the Earth is unique in the details of its development, certain elements are held in common, and knowledge and techniques gained in my work in eastern Canada may provide insight into the resolution of problems that geologists have in understanding other areas. My work is based on detailed examination of the rocks in the field in order to understand the distribution of the many different kinds of rocks that occur in the mountain belt (a process known as geological mapping). I collect representative samples and then in collaboration with colleagues who have the necessary equipment and expertise, I find out the ages of the rocks and determine their mineral and chemical compositions. I use all of these different types of information to make interpretations about what was happening in the mountain belt at the various times when each kind of rock was forming. Some features of the rocks, such as their isotopic compositions or magnetic and density characteristics, may help me to know what kinds of rocks underlie those that I see at the surface, information that will help me 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.
Program
Discovery Grants Program - Individual
Recipient
Location
Nova Scotia, Canada
Recipient Type
Academia
Type
Grant
Source
NSERC's Awards Data
As published
Application id
4230-2006
Name nom
Barr, Sandra
Department département
Geology
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
2006
Competition year année de concours
2006
Award amount
50200
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
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
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
1
Nb partie
5
Application title
Terrane provenance and evolution in the northern appalachian orogen
Keyword
NA
Application summary
Remnants of ancient mountain belts 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. This proposal focuses on understanding the separate distinct components (or "terranes") that came together to form the part of the Appalachian mountain belt in southern New Brunswick and Nova Scotia between about 650 and 350 million years ago. I want to figure out more exactly when the pieces came together, whether they came as numerous separate blocks or as a single composite block, and from where they came - possible source areas are any of the other continents, such as South America, Africa, and Scandinavia. Although each mountain belt on the Earth is unique in the details of its development, certain elements are held in common, and knowledge and techniques gained in my work in eastern Canada may provide insight into the resolution of problems that geologists have in understanding other areas. My work is based on detailed examination of the rocks in the field in order to understand the distribution of the many different kinds of rocks that occur in the mountain belt (a process known as geological mapping). I collect representative samples and then in collaboration with colleagues who have the necessary equipment and expertise, I find out the ages of the rocks and determine their mineral and chemical compositions. I use all of these different types of information to make interpretations about what was happening in the mountain belt at the various times when each kind of rock was forming. Some features of the rocks, such as their isotopic compositions or magnetic and density characteristics, may help me to know what kinds of rocks underlie those that I see at the surface, information that will help me 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.