Strain-Driven Elemental Re-Distribution during Hydration of the Mid-Lower Crust
Fluids are vital for the transport of mass and energy through the Earth’s crust and also for its thermodynamic re-equilibration in response to changes in pressure and temperature. Presented here are observations for the coupling between deformation and reaction, mass transport, and variations in tra...
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| Format: | Thesis |
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Curtin University
2020
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| Online Access: | http://hdl.handle.net/20.500.11937/79105 |
| _version_ | 1848764001751662592 |
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| author | Moore, Josephine |
| author_facet | Moore, Josephine |
| author_sort | Moore, Josephine |
| building | Curtin Institutional Repository |
| collection | Online Access |
| description | Fluids are vital for the transport of mass and energy through the Earth’s crust and also for its thermodynamic re-equilibration in response to changes in pressure and temperature. Presented here are observations for the coupling between deformation and reaction, mass transport, and variations in trace-element composition and isotope ratios. Overall, this thesis communicates the importance of mid- to lower crustal deformation for mass transfer and in the attainment of equilibria in the presence of fluid. |
| first_indexed | 2025-11-14T11:12:25Z |
| format | Thesis |
| id | curtin-20.500.11937-79105 |
| institution | Curtin University Malaysia |
| institution_category | Local University |
| last_indexed | 2025-11-14T11:12:25Z |
| publishDate | 2020 |
| publisher | Curtin University |
| recordtype | eprints |
| repository_type | Digital Repository |
| spelling | curtin-20.500.11937-791052020-05-13T06:25:52Z Strain-Driven Elemental Re-Distribution during Hydration of the Mid-Lower Crust Moore, Josephine Fluids are vital for the transport of mass and energy through the Earth’s crust and also for its thermodynamic re-equilibration in response to changes in pressure and temperature. Presented here are observations for the coupling between deformation and reaction, mass transport, and variations in trace-element composition and isotope ratios. Overall, this thesis communicates the importance of mid- to lower crustal deformation for mass transfer and in the attainment of equilibria in the presence of fluid. 2020 Thesis http://hdl.handle.net/20.500.11937/79105 Curtin University fulltext |
| spellingShingle | Moore, Josephine Strain-Driven Elemental Re-Distribution during Hydration of the Mid-Lower Crust |
| title | Strain-Driven Elemental Re-Distribution during Hydration of the Mid-Lower Crust |
| title_full | Strain-Driven Elemental Re-Distribution during Hydration of the Mid-Lower Crust |
| title_fullStr | Strain-Driven Elemental Re-Distribution during Hydration of the Mid-Lower Crust |
| title_full_unstemmed | Strain-Driven Elemental Re-Distribution during Hydration of the Mid-Lower Crust |
| title_short | Strain-Driven Elemental Re-Distribution during Hydration of the Mid-Lower Crust |
| title_sort | strain-driven elemental re-distribution during hydration of the mid-lower crust |
| url | http://hdl.handle.net/20.500.11937/79105 |