FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1434692241> ?p ?o ?g. }

• W1434692241 endingPage "745" @default.
• W1434692241 startingPage "728" @default.
• W1434692241 abstract "Submarine hydrothermal sulfide ores occur at mid-ocean ridges, intra-oceanic arcs and in back-arc basins associated with host rocks of highly variable composition. Pyrite is the dominant sulfide mineral in most samples presented within this study, and thus the trace element composition of pyrite may reflect the different metal sources and precipitation processes. Here, we report on a systematic study of minor and trace element contents in pyrite from active and inactive submarine hydrothermal vent fields at different plate-tectonic settings including the Indian and Mid-Atlantic Ridges, the Tonga–Kermadec intra-oceanic arc, the Lau back-arc and the central Okinawa Trough. Our results show that the trace element contents of pyrite from different locations vary significantly but for most elements without any systematic correlation to the concentration in the magmatic host rocks. Only As appears to be depleted in pyrite from ultramafic-hosted vent systems that are affected by serpentinization. These As depleted pyrites preferentially host Au 0 micro- or nano-particles. Bismuth is enriched in pyrite from hydrothermal systems that contain a sedimentary component and micro-inclusions of sphalerite are either due to fluid–sediment interaction or phase-separated fluid venting. Pyrites from individual locations have highly variable concentrations of elements like Au, Co, Cu, Se, Mo, Ag and Sb that are most likely related to fluid evolution and changes in fluid composition. Sub-seafloor hydrothermal fluid–seawater mixing influences the distribution of Au, Co, Cu, Se and Mo in pyrite. Elements like Au, Ag, Sb and Pb often have a characteristic affinity to As, while Cd correlates closely with Zn. A magmatic volatile contribution to the Hine Hina hydrothermal system may result in the precipitation of Cu-enriched pyrite. Our results show that the concentrations of most trace metals in pyrite are a function of the physicochemical parameters of the fluid phase rather than a reflection of the magmatic host rock composition." @default.
• W1434692241 created "2016-06-24" @default.
• W1434692241 creator A5012748078 @default.
• W1434692241 creator A5025452565 @default.
• W1434692241 creator A5055118307 @default.
• W1434692241 creator A5064629858 @default.
• W1434692241 creator A5083992192 @default.
• W1434692241 date "2016-01-01" @default.
• W1434692241 modified "2023-10-11" @default.
• W1434692241 title "Trace element systematics of pyrite from submarine hydrothermal vents" @default.
• W1434692241 cites W1541227778 @default.
• W1434692241 cites W1563105721 @default.
• W1434692241 cites W1575103472 @default.
• W1434692241 cites W1754089219 @default.
• W1434692241 cites W1963490192 @default.
• W1434692241 cites W1965693689 @default.
• W1434692241 cites W1965744338 @default.
• W1434692241 cites W1966750556 @default.
• W1434692241 cites W1966983664 @default.
• W1434692241 cites W1971307326 @default.
• W1434692241 cites W1971871518 @default.
• W1434692241 cites W1976819346 @default.
• W1434692241 cites W1976984795 @default.
• W1434692241 cites W1980608636 @default.
• W1434692241 cites W1988842153 @default.
• W1434692241 cites W1990822942 @default.
• W1434692241 cites W1991565667 @default.
• W1434692241 cites W1993317314 @default.
• W1434692241 cites W1993879904 @default.
• W1434692241 cites W1995419949 @default.
• W1434692241 cites W1995785490 @default.
• W1434692241 cites W1996135927 @default.
• W1434692241 cites W2001987411 @default.
• W1434692241 cites W2005000918 @default.
• W1434692241 cites W2007843418 @default.
• W1434692241 cites W2010989785 @default.
• W1434692241 cites W2015130957 @default.
• W1434692241 cites W2017264474 @default.
• W1434692241 cites W2017770619 @default.
• W1434692241 cites W2018093298 @default.
• W1434692241 cites W2019017051 @default.
• W1434692241 cites W2020468561 @default.
• W1434692241 cites W2025863397 @default.
• W1434692241 cites W2028917031 @default.
• W1434692241 cites W2029869957 @default.
• W1434692241 cites W2033804331 @default.
• W1434692241 cites W2037385914 @default.
• W1434692241 cites W2038614693 @default.
• W1434692241 cites W2042221220 @default.
• W1434692241 cites W2043710603 @default.
• W1434692241 cites W2044224264 @default.
• W1434692241 cites W2051323905 @default.
• W1434692241 cites W2053308667 @default.
• W1434692241 cites W2060363575 @default.
• W1434692241 cites W2061555440 @default.
• W1434692241 cites W2062957061 @default.
• W1434692241 cites W2065005729 @default.
• W1434692241 cites W2065128525 @default.
• W1434692241 cites W2066296869 @default.
• W1434692241 cites W2069412607 @default.
• W1434692241 cites W2070071554 @default.
• W1434692241 cites W2070075174 @default.
• W1434692241 cites W2076996184 @default.
• W1434692241 cites W2087448142 @default.
• W1434692241 cites W2087796207 @default.
• W1434692241 cites W2088096040 @default.
• W1434692241 cites W2090562875 @default.
• W1434692241 cites W2091027805 @default.
• W1434692241 cites W2092237459 @default.
• W1434692241 cites W2110799222 @default.
• W1434692241 cites W2111072199 @default.
• W1434692241 cites W2114955000 @default.
• W1434692241 cites W2116125238 @default.
• W1434692241 cites W2116294299 @default.
• W1434692241 cites W2125571496 @default.
• W1434692241 cites W2126621553 @default.
• W1434692241 cites W2128093883 @default.
• W1434692241 cites W2128405318 @default.
• W1434692241 cites W2137460333 @default.
• W1434692241 cites W2138675757 @default.
• W1434692241 cites W2148570407 @default.
• W1434692241 cites W2150457925 @default.
• W1434692241 cites W2154499471 @default.
• W1434692241 cites W2159868744 @default.
• W1434692241 cites W2256193665 @default.
• W1434692241 cites W2325843105 @default.
• W1434692241 doi "https://doi.org/10.1016/j.oregeorev.2015.07.012" @default.
• W1434692241 hasPublicationYear "2016" @default.
• W1434692241 type Work @default.
• W1434692241 sameAs 1434692241 @default.
• W1434692241 citedByCount "170" @default.
• W1434692241 countsByYear W14346922412016 @default.
• W1434692241 countsByYear W14346922412017 @default.
• W1434692241 countsByYear W14346922412018 @default.
• W1434692241 countsByYear W14346922412019 @default.
• W1434692241 countsByYear W14346922412020 @default.
• W1434692241 countsByYear W14346922412021 @default.
• W1434692241 countsByYear W14346922412022 @default.

• next