Physics
Scientist
Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia
A synthetic fluid inclusion study of copper solubility in hydrothermal brines from 525 to 725 °C and 0.3 to 1.7 GPa
Calculated hydrous granite solidi beyond the albite-jadeite transition
Low-temperature melt-fluid miscibility: Experimental evidence for enhanced mass transport in the upper crust by cooling fluids
Physical properties of hydrous magmas and related fluids and their role in mantle processes
Quantification of dehydration and mass fluxes from subducting slabs
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