Étude du comportement des éléments hautement sidérophiles et chalcophiles dans les gouttelettes sulfurées de MORB /

Patten, Clifford

doi:10.1522/030325504

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Mid-ocean Ridge Basalts (Morb)1

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2016

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“…MORB are formed by 10-20% partial melting, and are believed to be sulfur-saturated at their source (Keays, 1995;Mavrogenes and O"Neill, 1999). Thus, they commonly coexist with an exsolved sulfide melt that hosts most of their chalcophile and siderophile element budget, as in the pyroxenites (Patten, 2012;Patten et al, 2010;Peach et al, 1990).…”

Section: Mid-ocean Ridge Basalts (Morb)mentioning

confidence: 99%

“…A more recent study of MORB sulfides analysed trace-elements in six grains by LA-ICP-MS (Patten, 2012;Patten et al, 2010). The sulfides in this study were a combination of mss and isobaric solid solution (iss); similar to peridotite sulfides globally, but quite distinct from the typical pyroxenite-hosted sulfides (Andersen et al, 1987;Guo et al, 1999;Sen et al, 2010).…”

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confidence: 99%

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