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Research School of Earth Sciences, Australian National University, Canberra ACT, Australia. Research School of Earth Sciences, Australian National University, GPO Box 334, Canberra ACT 0200, Australia
Research School of Earth Sciences, Australian National University, Canberra, ACT 0200, Australia
Instituto de Geociências, Universidade de São Paulo, São Paulo SP 05508-080, Brazil; Research School of Earth Sciences, Australian National University, Canberra ACT 0200, Australia
Research School of Earth Sciences, Australian National University, Canberra ACT 0200, Australia
Australian National University, Research School of Earth Sciences, Australia; Institute of Geosciences, University of São Paulo, São Paulo, Brazil
An experimental study of the chalcophile character of Re: The effect of fO2, fS2 and temperature
Andean subduction-related lithospheric mantle: Growth and isotopic evidence of chemical exchange in mantle and crustal reservoirs
Andean subduction-related mantle xenoliths: isotopic evidence of Sr-Nd decoupling during metasomatism
Erratum to G. Mallmann, and H.St.C. O’Neill (2007) “The effect of oxygen fugacity on the partitioning of Re between crystals and silicate melt during mantle melting”, Geochimica et Cosmochimica Acta 71, 2837 2857
How chalcophile is rhenium? An experimental study of the solubility of Re in sulphide mattes
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