Lithofacies analysis of the Proterozoic Thelon Formation, Northwest Territories (including computer analysis of field data)
On the basis of a petrographic study of regionally distributed rock samples, the Proterozoic Thelon Formation, Northwest Territories, is here subdivided into four lithofacies. Clay-mineral studies and computer-aided assessment of field-notes substantiate these subdivisions, three of which can be pla...
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ftcarletonuniv:oai:curve.carleton.ca:29686 2023-05-15T17:46:36+02:00 Lithofacies analysis of the Proterozoic Thelon Formation, Northwest Territories (including computer analysis of field data) Cecile, Michael Peter 1973 https://curve.carleton.ca/11eac4a4-9fea-4fcd-8c18-d52c8c610b50 http://catalogue.library.carleton.ca/record=b1961526 https://doi.org/10.22215/etd/1973-12414 unknown https://curve.carleton.ca/11eac4a4-9fea-4fcd-8c18-d52c8c610b50 http://catalogue.library.carleton.ca/record=b1961526 https://doi.org/10.22215/etd/1973-12414 Thesis/Dissertation 1973 ftcarletonuniv https://doi.org/10.22215/etd/1973-12414 2022-01-23T08:13:48Z On the basis of a petrographic study of regionally distributed rock samples, the Proterozoic Thelon Formation, Northwest Territories, is here subdivided into four lithofacies. Clay-mineral studies and computer-aided assessment of field-notes substantiate these subdivisions, three of which can be placed in a vertical stratigraphic succession. Clay-mineral analysis, a study of quartz-grain types and review of the field data all indicate that quartz-rich sandstones of the Thelon Formation were derived mainly from kaolin-rich paleosols that were developed on granitoid and metamorphic rocks of the Churchill Structural Province. The petrologic and field data confirms a fining-upward trend, culminating with a marine transgression, as proposed by Donaldson (1967). In addition to recrystallized kaolinite, authigenic feldspar and diagenetic muscovites occur within the three main units of the Thelon Formation. The fourth subdivision, a petrographically distinct zone of possibly different age and/or origin, is characterized by alumina-rich dioctahedral chlorite in the sandstone matrix. Recognition of the subdivisions, and refinement of petrologic and clay-mineral data for the Thelon Formation, provide a basis for more detailed studies of other, possibly correlative, Proterozoic sandstone units in the Canadian Shield. Computer-processable field notes used in the study of field data were derived by conversion of the original field notes to a computable form. The system proved to be highly efficient, testifying to the potential of using field-note systems that are computer oriented. A field-note form was developed for future studies in the Thelon Basin and comparable Proterozoic basins, and recommendations for the use and derivation of computable field-note forms are presented herein. Thesis Northwest Territories CURVE - Carleton University Research Virtual Environment Northwest Territories Donaldson ENVELOPE(172.200,172.200,-84.617,-84.617) |
institution |
Open Polar |
collection |
CURVE - Carleton University Research Virtual Environment |
op_collection_id |
ftcarletonuniv |
language |
unknown |
description |
On the basis of a petrographic study of regionally distributed rock samples, the Proterozoic Thelon Formation, Northwest Territories, is here subdivided into four lithofacies. Clay-mineral studies and computer-aided assessment of field-notes substantiate these subdivisions, three of which can be placed in a vertical stratigraphic succession. Clay-mineral analysis, a study of quartz-grain types and review of the field data all indicate that quartz-rich sandstones of the Thelon Formation were derived mainly from kaolin-rich paleosols that were developed on granitoid and metamorphic rocks of the Churchill Structural Province. The petrologic and field data confirms a fining-upward trend, culminating with a marine transgression, as proposed by Donaldson (1967). In addition to recrystallized kaolinite, authigenic feldspar and diagenetic muscovites occur within the three main units of the Thelon Formation. The fourth subdivision, a petrographically distinct zone of possibly different age and/or origin, is characterized by alumina-rich dioctahedral chlorite in the sandstone matrix. Recognition of the subdivisions, and refinement of petrologic and clay-mineral data for the Thelon Formation, provide a basis for more detailed studies of other, possibly correlative, Proterozoic sandstone units in the Canadian Shield. Computer-processable field notes used in the study of field data were derived by conversion of the original field notes to a computable form. The system proved to be highly efficient, testifying to the potential of using field-note systems that are computer oriented. A field-note form was developed for future studies in the Thelon Basin and comparable Proterozoic basins, and recommendations for the use and derivation of computable field-note forms are presented herein. |
format |
Thesis |
author |
Cecile, Michael Peter |
spellingShingle |
Cecile, Michael Peter Lithofacies analysis of the Proterozoic Thelon Formation, Northwest Territories (including computer analysis of field data) |
author_facet |
Cecile, Michael Peter |
author_sort |
Cecile, Michael Peter |
title |
Lithofacies analysis of the Proterozoic Thelon Formation, Northwest Territories (including computer analysis of field data) |
title_short |
Lithofacies analysis of the Proterozoic Thelon Formation, Northwest Territories (including computer analysis of field data) |
title_full |
Lithofacies analysis of the Proterozoic Thelon Formation, Northwest Territories (including computer analysis of field data) |
title_fullStr |
Lithofacies analysis of the Proterozoic Thelon Formation, Northwest Territories (including computer analysis of field data) |
title_full_unstemmed |
Lithofacies analysis of the Proterozoic Thelon Formation, Northwest Territories (including computer analysis of field data) |
title_sort |
lithofacies analysis of the proterozoic thelon formation, northwest territories (including computer analysis of field data) |
publishDate |
1973 |
url |
https://curve.carleton.ca/11eac4a4-9fea-4fcd-8c18-d52c8c610b50 http://catalogue.library.carleton.ca/record=b1961526 https://doi.org/10.22215/etd/1973-12414 |
long_lat |
ENVELOPE(172.200,172.200,-84.617,-84.617) |
geographic |
Northwest Territories Donaldson |
geographic_facet |
Northwest Territories Donaldson |
genre |
Northwest Territories |
genre_facet |
Northwest Territories |
op_relation |
https://curve.carleton.ca/11eac4a4-9fea-4fcd-8c18-d52c8c610b50 http://catalogue.library.carleton.ca/record=b1961526 https://doi.org/10.22215/etd/1973-12414 |
op_doi |
https://doi.org/10.22215/etd/1973-12414 |
_version_ |
1766150335939739648 |