Spring geochemistry: a tool for mineral exploration in the South Nahanni River Basin, NWT
Bibliography: p. 136-152 Some pages are in colour. Geochemical data from over 200 springs within the remote 37,000 kms South Nahanni River Basin of the Mackenzie Mountains, Northwest Territories, were used to evaluate the economic mineral potential of the region which is proposed for a national park...
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ftunivcalgary:oai:prism.ucalgary.ca:1880/101835 2023-08-27T04:10:31+02:00 Spring geochemistry: a tool for mineral exploration in the South Nahanni River Basin, NWT Caron, Marie-Eve Ryan, M. Cathryn Grasby, Stephen E. 2007 xv, 152 leaves : ill. 30 cm. application/pdf http://hdl.handle.net/1880/101835 https://doi.org/10.11575/PRISM/834 eng eng University of Calgary Calgary Caron, M. (2007). Spring geochemistry: a tool for mineral exploration in the South Nahanni River Basin, NWT (Unpublished master's thesis). University of Calgary, Calgary, AB. doi:10.11575/PRISM/834 http://dx.doi.org/10.11575/PRISM/834 http://hdl.handle.net/1880/101835 University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. master thesis 2007 ftunivcalgary https://doi.org/10.11575/PRISM/834 2023-08-06T06:20:38Z Bibliography: p. 136-152 Some pages are in colour. Geochemical data from over 200 springs within the remote 37,000 kms South Nahanni River Basin of the Mackenzie Mountains, Northwest Territories, were used to evaluate the economic mineral potential of the region which is proposed for a national park designation. Trace element analyses were evaluated using three different approaches (the sum of trace element concentrations as a percentage of total dissolved solids, identifying individual elevated trace elements, and the inverse use of the Ficklin Diagram). Two out of the three approaches detected the two known deposits of the area, Prairie Creek and Tungsten, but not with the same method in each case, indicating that a multi-pronged approach is best. The springs are elevated in trace elements in comparison to mineral deposit related waters around the world. Silica geothermometry determined the average depth of circulation of the springs to be 2.1 km in the warm or hot springs and ranging from 4. 7 km to less than 200 m for the entire dataset, indicative of the accessibility of the predicted mineralized zones. These simple statistical and graphing methods can identify mineralized zones quickly and efficiently in a largely under-explored area. Master Thesis Mackenzie mountains Northwest Territories South Nahanni River PRISM - University of Calgary Digital Repository Northwest Territories South Nahanni River ENVELOPE(-123.353,-123.353,61.050,61.050) |
institution |
Open Polar |
collection |
PRISM - University of Calgary Digital Repository |
op_collection_id |
ftunivcalgary |
language |
English |
description |
Bibliography: p. 136-152 Some pages are in colour. Geochemical data from over 200 springs within the remote 37,000 kms South Nahanni River Basin of the Mackenzie Mountains, Northwest Territories, were used to evaluate the economic mineral potential of the region which is proposed for a national park designation. Trace element analyses were evaluated using three different approaches (the sum of trace element concentrations as a percentage of total dissolved solids, identifying individual elevated trace elements, and the inverse use of the Ficklin Diagram). Two out of the three approaches detected the two known deposits of the area, Prairie Creek and Tungsten, but not with the same method in each case, indicating that a multi-pronged approach is best. The springs are elevated in trace elements in comparison to mineral deposit related waters around the world. Silica geothermometry determined the average depth of circulation of the springs to be 2.1 km in the warm or hot springs and ranging from 4. 7 km to less than 200 m for the entire dataset, indicative of the accessibility of the predicted mineralized zones. These simple statistical and graphing methods can identify mineralized zones quickly and efficiently in a largely under-explored area. |
author2 |
Ryan, M. Cathryn Grasby, Stephen E. |
format |
Master Thesis |
author |
Caron, Marie-Eve |
spellingShingle |
Caron, Marie-Eve Spring geochemistry: a tool for mineral exploration in the South Nahanni River Basin, NWT |
author_facet |
Caron, Marie-Eve |
author_sort |
Caron, Marie-Eve |
title |
Spring geochemistry: a tool for mineral exploration in the South Nahanni River Basin, NWT |
title_short |
Spring geochemistry: a tool for mineral exploration in the South Nahanni River Basin, NWT |
title_full |
Spring geochemistry: a tool for mineral exploration in the South Nahanni River Basin, NWT |
title_fullStr |
Spring geochemistry: a tool for mineral exploration in the South Nahanni River Basin, NWT |
title_full_unstemmed |
Spring geochemistry: a tool for mineral exploration in the South Nahanni River Basin, NWT |
title_sort |
spring geochemistry: a tool for mineral exploration in the south nahanni river basin, nwt |
publisher |
University of Calgary |
publishDate |
2007 |
url |
http://hdl.handle.net/1880/101835 https://doi.org/10.11575/PRISM/834 |
long_lat |
ENVELOPE(-123.353,-123.353,61.050,61.050) |
geographic |
Northwest Territories South Nahanni River |
geographic_facet |
Northwest Territories South Nahanni River |
genre |
Mackenzie mountains Northwest Territories South Nahanni River |
genre_facet |
Mackenzie mountains Northwest Territories South Nahanni River |
op_relation |
Caron, M. (2007). Spring geochemistry: a tool for mineral exploration in the South Nahanni River Basin, NWT (Unpublished master's thesis). University of Calgary, Calgary, AB. doi:10.11575/PRISM/834 http://dx.doi.org/10.11575/PRISM/834 http://hdl.handle.net/1880/101835 |
op_rights |
University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. |
op_doi |
https://doi.org/10.11575/PRISM/834 |
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1775352623994503168 |