Geology Ward Inlet North Baffin Island Nunavut Nts 25 O North
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Geology Ward Inlet North Baffin Island Nunavut Nts 25 O North
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Author :
language : en
Publisher:
Release Date : 2016
Geology Ward Inlet North Baffin Island Nunavut Nts 25 O North written by and has been published by this book supported file pdf, txt, epub, kindle and other format this book has been release on 2016 with categories.
The Hall Peninsula Integrated Geoscience Program was led by the Canada-Nunavut Geoscience Office, and was designed to increase the geoscience knowledge and assess the economic potential of the area. Eastern Hall Peninsula is dominantly underlain by Archean tonalite to quartz diorite orthogneiss, while Paleoproterozoic supracrustal and intrusive rocks are exposed to the west. The supracrustal rocks are dominated by pelitic, psammitic, amphibolite and calc-silicate units, are interpreted as correlative with the Lake Harbour Group, and are cut by granulite-grade monzogranite to diorite intrusions. Hall Peninsula records three phases of metamorphism and deformation associated with the Trans-Hudson Orogen that have produced thick-skinned, east-verging fold and thrust structures and amphibolite to granulite facies mineral assemblages. Hall Peninsula hosts a highly prospective diamond kimberlite field, as well as mafic and carbonate supracrustal rocks, and ultramafic intrusions that may contain base and/or precious metal, semi-precious gemstone and carving stone resource potential.
Geology Ward Inlet North Baffin Island Nunavut Nts 25 O North
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Author :
language : en
Publisher:
Release Date : 2016
Geology Ward Inlet North Baffin Island Nunavut Nts 25 O North written by and has been published by this book supported file pdf, txt, epub, kindle and other format this book has been release on 2016 with categories.
The Hall Peninsula Integrated Geoscience Program was led by the Canada-Nunavut Geoscience Office, and was designed to increase the geoscience knowledge and assess the economic potential of the area. Eastern Hall Peninsula is dominantly underlain by Archean tonalite to quartz diorite orthogneiss, while Paleoproterozoic supracrustal and intrusive rocks are exposed to the west. The supracrustal rocks are dominated by pelitic, psammitic, amphibolite and calc-silicate units, are interpreted as correlative with the Lake Harbour Group, and are cut by granulite-grade monzogranite to diorite intrusions. Hall Peninsula records three phases of metamorphism and deformation associated with the Trans-Hudson Orogen that have produced thick-skinned, east-verging fold and thrust structures and amphibolite to granulite facies mineral assemblages. Hall Peninsula hosts a highly prospective diamond kimberlite field, as well as mafic and carbonate supracrustal rocks, and ultramafic intrusions that may contain base and/or precious metal, semi-precious gemstone and carving stone resource potential.
Geology Ward Inlet South Baffin Island Nunavut Nts 25 O South And Nts 25 J Part
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Author :
language : en
Publisher:
Release Date : 2016
Geology Ward Inlet South Baffin Island Nunavut Nts 25 O South And Nts 25 J Part written by and has been published by this book supported file pdf, txt, epub, kindle and other format this book has been release on 2016 with categories.
The Hall Peninsula Integrated Geoscience Program was led by the Canada-Nunavut Geoscience Office, and was designed to increase the geoscience knowledge and assess the economic potential of the area. Eastern Hall Peninsula is dominantly underlain by Archean tonalite to quartz diorite orthogneiss, while Paleoproterozoic supracrustal and intrusive rocks are exposed to the west. The supracrustal rocks are dominated by pelitic, psammitic, amphibolite and calc-silicate units, are interpreted as correlative with the Lake Harbour Group, and are cut by granulite-grade monzogranite to diorite intrusions. Hall Peninsula records three phases of metamorphism and deformation associated with the Trans-Hudson Orogen that have produced thick-skinned, east-verging fold and thrust structures and amphibolite to granulite facies mineral assemblages. Hall Peninsula hosts a highly prospective diamond kimberlite field, as well as mafic and carbonate supracrustal rocks, and ultramafic intrusions that may contain base and/or precious metal, semi-precious gemstone and carving stone resource potential.
Geology Ward Inlet South Baffin Island Nunavut Nts 25 O South And Nts 25 J Part
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Author :
language : en
Publisher:
Release Date : 2016
Geology Ward Inlet South Baffin Island Nunavut Nts 25 O South And Nts 25 J Part written by and has been published by this book supported file pdf, txt, epub, kindle and other format this book has been release on 2016 with categories.
The Hall Peninsula Integrated Geoscience Program was led by the Canada-Nunavut Geoscience Office, and was designed to increase the geoscience knowledge and assess the economic potential of the area. Eastern Hall Peninsula is dominantly underlain by Archean tonalite to quartz diorite orthogneiss, while Paleoproterozoic supracrustal and intrusive rocks are exposed to the west. The supracrustal rocks are dominated by pelitic, psammitic, amphibolite and calc-silicate units, are interpreted as correlative with the Lake Harbour Group, and are cut by granulite-grade monzogranite to diorite intrusions. Hall Peninsula records three phases of metamorphism and deformation associated with the Trans-Hudson Orogen that have produced thick-skinned, east-verging fold and thrust structures and amphibolite to granulite facies mineral assemblages. Hall Peninsula hosts a highly prospective diamond kimberlite field, as well as mafic and carbonate supracrustal rocks, and ultramafic intrusions that may contain base and/or precious metal, semi-precious gemstone and carving stone resource potential.
Geology Beekman Peninsula North Baffin Island Nunavut Nts 25 P North And Nts 15 M Part
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Author : H. M. Steenkamp
language : en
Publisher:
Release Date : 2016
Geology Beekman Peninsula North Baffin Island Nunavut Nts 25 P North And Nts 15 M Part written by H. M. Steenkamp and has been published by this book supported file pdf, txt, epub, kindle and other format this book has been release on 2016 with categories.
Geology Of The Clyde Cockburn Land Map Area North Central Baffin Island Nunavut
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Author : G. D. Jackson
language : en
Publisher:
Release Date : 2000
Geology Of The Clyde Cockburn Land Map Area North Central Baffin Island Nunavut written by G. D. Jackson and has been published by this book supported file pdf, txt, epub, kindle and other format this book has been release on 2000 with Geology categories.
Describes the geology of an area covering about 82,000 square kilometres in north central Baffin Island, beginning with an introduction on the area's location, access, physiography, climate, general geology, and previous studies. Subsequent chapters cover the geology of the Archean to Cretaceous and Recent formations, regional geochemistry, regional geochronology, regional & contact metamorphism, economic geology, and structural geology. The final chapter is a regional synthesis with general comments on structural subdivisions, the nature of their boundaries, regional correlations, and geological history.
Surficial Geology Milne Inlet Baffin Island Nunavut Nts 48 A
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Author : Geological Survey of Canada
language : en
Publisher:
Release Date : 2018
Surficial Geology Milne Inlet Baffin Island Nunavut Nts 48 A written by Geological Survey of Canada and has been published by this book supported file pdf, txt, epub, kindle and other format this book has been release on 2018 with categories.
Geology Beekman Peninsula North Baffin Island Nunavut Nts 25 P North And Nts 15 M Part
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Author :
language : en
Publisher:
Release Date : 2016
Geology Beekman Peninsula North Baffin Island Nunavut Nts 25 P North And Nts 15 M Part written by and has been published by this book supported file pdf, txt, epub, kindle and other format this book has been release on 2016 with categories.
The Hall Peninsula Integrated Geoscience Program was led by the Canada-Nunavut Geoscience Office, and was designed to increase the geoscience knowledge and assess the economic potential of the area. Eastern Hall Peninsula is dominantly underlain by Archean tonalite to quartz diorite orthogneiss, while Paleoproterozoic supracrustal and intrusive rocks are exposed to the west. The supracrustal rocks are dominated by pelitic, psammitic, amphibolite and calc-silicate units, are interpreted as correlative with the Lake Harbour Group, and are cut by granulite-grade monzogranite to diorite intrusions. Hall Peninsula records three phases of metamorphism and deformation associated with the Trans-Hudson Orogen that have produced thickskinned, east-verging fold and thrust structures and amphibolite to granulite facies mineral assemblages. Hall Peninsula hosts a highly prospective diamond kimberlite field, as well as mafic and carbonate supracrustal rocks, and ultramafic intrusions that may contain base and/or precious metal, semi-precious gemstone and carving stone resource potential.
Surficial Geology Ward Inlet Baffin Island Nunavut
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Author :
language : en
Publisher:
Release Date : 2014
Surficial Geology Ward Inlet Baffin Island Nunavut written by and has been published by this book supported file pdf, txt, epub, kindle and other format this book has been release on 2014 with categories.
Geology Loks Land Baffin Island Nunavut Nts 25 I Part
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Author :
language : en
Publisher:
Release Date : 2016
Geology Loks Land Baffin Island Nunavut Nts 25 I Part written by and has been published by this book supported file pdf, txt, epub, kindle and other format this book has been release on 2016 with categories.
The Hall Peninsula Integrated Geoscience Program was led by the Canada-Nunavut Geoscience Office, and was designed to increase the geoscience knowledge and assess the economic potential of the area. Eastern Hall Peninsula is dominantly underlain by Archean tonalite to quartz diorite orthogneiss, while Paleoproterozoic supracrustal and intrusive rocks are exposed to the west. The supracrustal rocks are dominated by pelitic, psammitic, amphibolite and calc-silicate units, are interpreted as correlative with the Lake Harbour Group, and are cut by granulite-grade monzogranite to diorite intrusions. Hall Peninsula records three phases of metamorphism and deformation associated with the Trans-Hudson Orogen that have produced thick-skinned, east-verging fold and thrust structures and amphibolite to granulite facies mineral assemblages. Hall Peninsula hosts a highly prospective diamond kimberlite field, as well as mafic and carbonate supracrustal rocks, and ultramafic intrusions that may contain base and/or precious metal, semi-precious gemstone and carving stone resource potential.