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• W2319056662 endingPage "367" @default.
• W2319056662 startingPage "305" @default.
• W2319056662 abstract "The highly siderophile elements (HSE) consist of the Platinum Group Elements (PGE: Ru, Rh, Pd, Os, Ir, Pt) along with rhenium and gold. These transition elements show relative chemical inertness and high market values, which respectively earned them the additional names of noble metals and precious metals.The HSE show a very pronounced affinity for iron metal, which translates into metal/silicate partition coefficients similar to or higher than 10,000 over large ranges of both pressure and temperature (e.g., O’Neill et al. 1995; Borisov and Palme 2000; Ertel et al. 1999, 2001, 2006, 2008; Fortenfant et al. 2003, 2006; Brenan et al. 2005; Cottrell and Walker 2006; Brenan and McDonough 2009; Laurenz et al. 2010; Mann et al. 2012; see Brenan et al. 2016, this volume for detailed review). Consequently, the HSE are thought to have been efficiently sequestered within the metallic core of our planet during the metal–silicate differentiation of Earth, leaving the silicate counterpart almost HSE-barren. Investigations of mantle peridotites since the 1970s revealed ng.g−1 level abundances as well as close-to-chondritic proportions of the HSE (Chou 1978; Jagoutz et al. 1979; Mitchell and Keays 1981; McDonough and Sun 1995; Becker et al. 2006; Fischer-Godde et al. 2011). Such abundances and inter-HSE fractionations are not predicted for the silicate Earth left after separation of the metallic core for low- or high-pressure core–mantle differentiation (see Brenan et al. 2016, this volume). The close agreement between the osmium isotopic compositions of fertile mantle peridotites and those of chondritic meteorites (Walker et al. 2002a), which requires nearly identical Re/Os ratios in these two reservoirs, provides particularly convincing evidence that the mantle’s HSE content cannot simply represent the residue left after core formation. …" @default.
• W2319056662 created "2016-06-24" @default.
• W2319056662 creator A5013329708 @default.
• W2319056662 creator A5066484590 @default.
• W2319056662 date "2015-12-14" @default.
• W2319056662 modified "2023-10-17" @default.
• W2319056662 title "Highly Siderophile Element and¹⁸⁷Os Signatures in Non-cratonic Basalt-hosted Peridotite Xenoliths: Unravelling the Origin and Evolution of the Post-Archean Lithospheric Mantle" @default.
• W2319056662 cites W1481344554 @default.
• W2319056662 cites W1497121464 @default.
• W2319056662 cites W1498344923 @default.
• W2319056662 cites W1509335520 @default.
• W2319056662 cites W1654280627 @default.
• W2319056662 cites W1717599307 @default.
• W2319056662 cites W1964324070 @default.
• W2319056662 cites W1964668579 @default.
• W2319056662 cites W1965660752 @default.
• W2319056662 cites W1966540505 @default.
• W2319056662 cites W1966841416 @default.
• W2319056662 cites W1967145848 @default.
• W2319056662 cites W1968554206 @default.
• W2319056662 cites W1968605693 @default.
• W2319056662 cites W1969840459 @default.
• W2319056662 cites W1969859799 @default.
• W2319056662 cites W1970494800 @default.
• W2319056662 cites W1970527462 @default.
• W2319056662 cites W1970771915 @default.
• W2319056662 cites W1971419367 @default.
• W2319056662 cites W1972437778 @default.
• W2319056662 cites W1974064481 @default.
• W2319056662 cites W1976252713 @default.
• W2319056662 cites W1976265423 @default.
• W2319056662 cites W1977457396 @default.
• W2319056662 cites W1977811562 @default.
• W2319056662 cites W1980528605 @default.
• W2319056662 cites W1981977799 @default.
• W2319056662 cites W1984745359 @default.
• W2319056662 cites W1984787349 @default.
• W2319056662 cites W1985787129 @default.
• W2319056662 cites W1986681125 @default.
• W2319056662 cites W1986713906 @default.
• W2319056662 cites W1986744113 @default.
• W2319056662 cites W1987112298 @default.
• W2319056662 cites W1987531220 @default.
• W2319056662 cites W1988599392 @default.
• W2319056662 cites W1988694196 @default.
• W2319056662 cites W1990613251 @default.
• W2319056662 cites W1991894787 @default.
• W2319056662 cites W1992704749 @default.
• W2319056662 cites W1993284636 @default.
• W2319056662 cites W1994283252 @default.
• W2319056662 cites W1994537115 @default.
• W2319056662 cites W1995798238 @default.
• W2319056662 cites W1996038144 @default.
• W2319056662 cites W1997218517 @default.
• W2319056662 cites W1998125513 @default.
• W2319056662 cites W1999710591 @default.
• W2319056662 cites W1999922408 @default.
• W2319056662 cites W1999985630 @default.
• W2319056662 cites W2000593660 @default.
• W2319056662 cites W2000857709 @default.
• W2319056662 cites W2001397154 @default.
• W2319056662 cites W2001426318 @default.
• W2319056662 cites W2001463300 @default.
• W2319056662 cites W2001989120 @default.
• W2319056662 cites W2003371840 @default.
• W2319056662 cites W2003668450 @default.
• W2319056662 cites W2004789205 @default.
• W2319056662 cites W2005237558 @default.
• W2319056662 cites W2007551255 @default.
• W2319056662 cites W2007790835 @default.
• W2319056662 cites W2008297722 @default.
• W2319056662 cites W2008489622 @default.
• W2319056662 cites W2009876973 @default.
• W2319056662 cites W2010056906 @default.
• W2319056662 cites W2010659865 @default.
• W2319056662 cites W2011176927 @default.
• W2319056662 cites W2011250343 @default.
• W2319056662 cites W2013213907 @default.
• W2319056662 cites W2014406426 @default.
• W2319056662 cites W2015258641 @default.
• W2319056662 cites W2015644466 @default.
• W2319056662 cites W2016893657 @default.
• W2319056662 cites W2017242228 @default.
• W2319056662 cites W2017267832 @default.
• W2319056662 cites W2017515683 @default.
• W2319056662 cites W2017577740 @default.
• W2319056662 cites W2017716598 @default.
• W2319056662 cites W2018518478 @default.
• W2319056662 cites W2019082012 @default.
• W2319056662 cites W2019339918 @default.
• W2319056662 cites W2019894721 @default.
• W2319056662 cites W2020947023 @default.
• W2319056662 cites W2021696687 @default.
• W2319056662 cites W2021832532 @default.
• W2319056662 cites W2021869346 @default.
• W2319056662 cites W2022272868 @default.
• W2319056662 cites W2022897365 @default.
• W2319056662 cites W2024825839 @default.

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