2012
DOI: 10.1016/j.gca.2012.01.026
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Partitioning of Ru, Rh, Pd, Re, Ir and Pt between liquid metal and silicate at high pressures and high temperatures - Implications for the origin of highly siderophile element concentrations in the Earth’s mantle

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Cited by 149 publications
(167 citation statements)
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References 53 publications
(132 reference statements)
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“…In studies that assume only the presence of quench related inclusions, there is variable agreement with the inclusion-free data. For example, good agreement is observed with the results of Mann et al 49 , however, the experiments of Cottrell et al 22 display systematically lower values of D Met/Sil than inclusion-free experiments 31 . The generation of inclusion-free experiments at a wide range of conditions is thus crucial to assess the reliability of previous inclusion-contaminated measurements.…”
Section: Discussionsupporting
confidence: 74%
See 1 more Smart Citation
“…In studies that assume only the presence of quench related inclusions, there is variable agreement with the inclusion-free data. For example, good agreement is observed with the results of Mann et al 49 , however, the experiments of Cottrell et al 22 display systematically lower values of D Met/Sil than inclusion-free experiments 31 . The generation of inclusion-free experiments at a wide range of conditions is thus crucial to assess the reliability of previous inclusion-contaminated measurements.…”
Section: Discussionsupporting
confidence: 74%
“…For experiments in which the HSE of interest is not present as a pure phase (i.e., HSE metal activity <1), concentrations measured in the silicate phase are corrected to unit activity using available thermodynamic data. With the exception of Au, a useful summary of the available activity-composition relations for HSE alloys is provided in reference 49 . Limited data for Au-Fe alloys may be found in references 46,51 …”
Section: Discussionmentioning
confidence: 99%
“…Furthermore, neither Zr nor Ba are siderophile elements (Mo only slightly so), nor are they strongly separated between the gas and solid phases. Recently, Mann et al (2012) have shown that Ru was not partitioned, not even under high pressure or temperature. Both Mo and Zr are refractory elements and even though Ba is less refractory, it is still far from being volatile.…”
Section: Presolar Grainsmentioning
confidence: 99%
“…The principal evidence for such late material addition comes from the concentrations of highly siderophile elements (HSE: e.g. Os, Pt, Re, Au) in Earth's mantle, which are higher than expected for metal-silicate equilibration during core formation (Brenan and McDonough, 2009;Mann et al, 2012). Moreover, the HSE in the mantle occur in broadly chondritic relative proportions, which is unexpected for metal-silicate partitioning (Meisel et al, 1996;Becker et al, 2006).…”
Section: Introductionmentioning
confidence: 99%