Mineral Geochemistry, Deformation and Ore Fluid Evolution in the Capricorn Orogen, WA
The Capricorn Orogen, Western Australia, has a complex history spanning over a billion years. Regional deformation, metamorphism and magmatism has induced migration of ore fluids into local ore deposits. Mineral geochemistry records the chemical environment of ore precipitation and is employed to de...
| Main Author: | |
|---|---|
| Format: | Thesis |
| Published: |
Curtin University
2017
|
| Online Access: | http://hdl.handle.net/20.500.11937/69391 |
| _version_ | 1848762038339239936 |
|---|---|
| author | Meadows, Holly Rachael |
| author_facet | Meadows, Holly Rachael |
| author_sort | Meadows, Holly Rachael |
| building | Curtin Institutional Repository |
| collection | Online Access |
| description | The Capricorn Orogen, Western Australia, has a complex history spanning over a billion years. Regional deformation, metamorphism and magmatism has induced migration of ore fluids into local ore deposits. Mineral geochemistry records the chemical environment of ore precipitation and is employed to determine the source of fluids and age of mineral growth. Integration of mineral geochemistry into complex geological systems is used to identify overprinting fluid and deformation events, and evaluate the formation of ore. |
| first_indexed | 2025-11-14T10:41:13Z |
| format | Thesis |
| id | curtin-20.500.11937-69391 |
| institution | Curtin University Malaysia |
| institution_category | Local University |
| last_indexed | 2025-11-14T10:41:13Z |
| publishDate | 2017 |
| publisher | Curtin University |
| recordtype | eprints |
| repository_type | Digital Repository |
| spelling | curtin-20.500.11937-693912018-08-03T02:26:30Z Mineral Geochemistry, Deformation and Ore Fluid Evolution in the Capricorn Orogen, WA Meadows, Holly Rachael The Capricorn Orogen, Western Australia, has a complex history spanning over a billion years. Regional deformation, metamorphism and magmatism has induced migration of ore fluids into local ore deposits. Mineral geochemistry records the chemical environment of ore precipitation and is employed to determine the source of fluids and age of mineral growth. Integration of mineral geochemistry into complex geological systems is used to identify overprinting fluid and deformation events, and evaluate the formation of ore. 2017 Thesis http://hdl.handle.net/20.500.11937/69391 Curtin University fulltext |
| spellingShingle | Meadows, Holly Rachael Mineral Geochemistry, Deformation and Ore Fluid Evolution in the Capricorn Orogen, WA |
| title | Mineral Geochemistry, Deformation and Ore Fluid Evolution in the Capricorn Orogen, WA |
| title_full | Mineral Geochemistry, Deformation and Ore Fluid Evolution in the Capricorn Orogen, WA |
| title_fullStr | Mineral Geochemistry, Deformation and Ore Fluid Evolution in the Capricorn Orogen, WA |
| title_full_unstemmed | Mineral Geochemistry, Deformation and Ore Fluid Evolution in the Capricorn Orogen, WA |
| title_short | Mineral Geochemistry, Deformation and Ore Fluid Evolution in the Capricorn Orogen, WA |
| title_sort | mineral geochemistry, deformation and ore fluid evolution in the capricorn orogen, wa |
| url | http://hdl.handle.net/20.500.11937/69391 |