FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2567424871> ?p ?o ?g. }

• W2567424871 endingPage "77" @default.
• W2567424871 startingPage "67" @default.
• W2567424871 abstract "Abstract Immiscible sulphide liquids preserved as magmatic sulphide globules are hosted in igneous rocks of highly variable composition formed during magmatic processes at different tectonic settings. Here we report on compositional in situ data of magmatic sulphides from mid-ocean ridge, back-arc and island arc magmatic systems. Iron-Ni-rich monosulphide solid solutions (mss) that mainly consist of pyrrhotite and pentlandite are the dominant phases in magmatic sulphide globules. In subduction-related magmas mss are most abundant in relatively evolved melts and characterised by low Ni and high Fe contents, as well as low Ni/Cu ratios (  1). Thus, mss chemistry varies systematically in lavas from the different tectonic settings in terms of their Fe-Ni distribution and Ni/Cu ratio. The observed mineralogical and chemical variations between mss from the different settings reflect early S saturation accompanied by olivine fractionation along mid-ocean ridges compared to later stage S saturation in arc systems associated with Fe-Ti oxide fractionation. These systematics are probably related to the relatively oxidised character of subduction zone magmas opposed to more reduced mid-ocean ridge melts. Large Ni/Cu variations in mss from the same locality and in individual samples suggest that S saturation is a multistage or continuous process leading to inclusions of magmatic sulphides that represent different fractionation stages in the ascending magma." @default.
• W2567424871 created "2017-01-06" @default.
• W2567424871 creator A5012748078 @default.
• W2567424871 creator A5025452565 @default.
• W2567424871 creator A5035849903 @default.
• W2567424871 creator A5064629858 @default.
• W2567424871 creator A5083992192 @default.
• W2567424871 date "2017-02-01" @default.
• W2567424871 modified "2023-09-26" @default.
• W2567424871 title "Systematic variations in magmatic sulphide chemistry from mid-ocean ridges, back-arc basins and island arcs" @default.
• W2567424871 cites W1434692241 @default.
• W2567424871 cites W1541227778 @default.
• W2567424871 cites W1640047074 @default.
• W2567424871 cites W1893068022 @default.
• W2567424871 cites W1963590813 @default.
• W2567424871 cites W1971307326 @default.
• W2567424871 cites W1972729527 @default.
• W2567424871 cites W1976984795 @default.
• W2567424871 cites W1986713906 @default.
• W2567424871 cites W1987275845 @default.
• W2567424871 cites W1988842153 @default.
• W2567424871 cites W1993490923 @default.
• W2567424871 cites W1995798238 @default.
• W2567424871 cites W1999323899 @default.
• W2567424871 cites W1999502028 @default.
• W2567424871 cites W2003331679 @default.
• W2567424871 cites W2004384593 @default.
• W2567424871 cites W2005141427 @default.
• W2567424871 cites W2010094459 @default.
• W2567424871 cites W2011599012 @default.
• W2567424871 cites W2011753735 @default.
• W2567424871 cites W2014763366 @default.
• W2567424871 cites W2017070614 @default.
• W2567424871 cites W2032710581 @default.
• W2567424871 cites W2032800272 @default.
• W2567424871 cites W2035297658 @default.
• W2567424871 cites W2052641018 @default.
• W2567424871 cites W2054002371 @default.
• W2567424871 cites W2062104243 @default.
• W2567424871 cites W2065489771 @default.
• W2567424871 cites W2068044270 @default.
• W2567424871 cites W2068421286 @default.
• W2567424871 cites W2074054545 @default.
• W2567424871 cites W2074062071 @default.
• W2567424871 cites W2076702980 @default.
• W2567424871 cites W2078697196 @default.
• W2567424871 cites W2081723971 @default.
• W2567424871 cites W2083567169 @default.
• W2567424871 cites W2087673255 @default.
• W2567424871 cites W2087796207 @default.
• W2567424871 cites W2088516428 @default.
• W2567424871 cites W2100582229 @default.
• W2567424871 cites W2109221183 @default.
• W2567424871 cites W2111173087 @default.
• W2567424871 cites W2111798811 @default.
• W2567424871 cites W2116294299 @default.
• W2567424871 cites W2117240630 @default.
• W2567424871 cites W2119091455 @default.
• W2567424871 cites W2121755657 @default.
• W2567424871 cites W2123260607 @default.
• W2567424871 cites W2128405318 @default.
• W2567424871 cites W2140001621 @default.
• W2567424871 cites W2148418693 @default.
• W2567424871 cites W2163156840 @default.
• W2567424871 cites W2167448438 @default.
• W2567424871 cites W2220306744 @default.
• W2567424871 cites W2276480568 @default.
• W2567424871 cites W2325944355 @default.
• W2567424871 cites W2483393773 @default.
• W2567424871 cites W2508973363 @default.
• W2567424871 cites W2510116043 @default.
• W2567424871 cites W965761834 @default.
• W2567424871 doi "https://doi.org/10.1016/j.chemgeo.2016.12.028" @default.
• W2567424871 hasPublicationYear "2017" @default.
• W2567424871 type Work @default.
• W2567424871 sameAs 2567424871 @default.
• W2567424871 citedByCount "31" @default.
• W2567424871 countsByYear W25674248712018 @default.
• W2567424871 countsByYear W25674248712019 @default.
• W2567424871 countsByYear W25674248712020 @default.
• W2567424871 countsByYear W25674248712021 @default.
• W2567424871 countsByYear W25674248712022 @default.
• W2567424871 countsByYear W25674248712023 @default.
• W2567424871 crossrefType "journal-article" @default.
• W2567424871 hasAuthorship W2567424871A5012748078 @default.
• W2567424871 hasAuthorship W2567424871A5025452565 @default.
• W2567424871 hasAuthorship W2567424871A5035849903 @default.
• W2567424871 hasAuthorship W2567424871A5064629858 @default.
• W2567424871 hasAuthorship W2567424871A5083992192 @default.
• W2567424871 hasConcept C111368507 @default.
• W2567424871 hasConcept C127313418 @default.
• W2567424871 hasConcept C151730666 @default.
• W2567424871 hasConcept C1965285 @default.
• W2567424871 hasConcept C2524010 @default.
• W2567424871 hasConcept C33923547 @default.
• W2567424871 hasConcept C58097730 @default.
• W2567424871 hasConcept C63379926 @default.
• W2567424871 hasConcept C77928131 @default.

• next