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dc.contributor.authorMoore, Josephine
dc.contributor.supervisorAndrew Putnisen_US
dc.contributor.supervisorAndreas Beinlichen_US

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.

dc.publisherCurtin Universityen_US
dc.titleStrain-Driven Elemental Re-Distribution during Hydration of the Mid-Lower Crusten_US
curtin.departmentSchool of Earth and Planetary Sciencesen_US
curtin.departmentThe Institute for Geoscience Researchen_US
curtin.accessStatusOpen accessen_US
curtin.facultyScience and Engineeringen_US
curtin.contributor.orcidMoore, Josephine [0000-0003-1842-5595]en_US

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