FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2012154227> ?p ?o ?g. }

• W2012154227 endingPage "187" @default.
• W2012154227 startingPage "178" @default.
• W2012154227 abstract "Abstract The depletion of high field strength elements such as Zr, Nb and Ta is a characteristic feature of arc magmas and it has been attributed to a low solubility of these elements in slab-derived aqueous fluids. We have determined zircon solubility in aqueous fluids up to 1025 °C and 20 kbar by in situ observation of dissolving zircon grains in the hydrothermal diamond anvil cell. Zircon solubilities in H2O with silica activity buffered by quartz are very low, from 1.0 to 3.3 ppm Zr, and weakly increase with temperature and pressure. Experimental results were fitted to the following fluid density model: log c ( ± 0.10 ) = ( 3.45 ± 0.92 ) - ( 3803 ± 1098 ) T - 1 + ( 1.52 ± 0.63 ) log ρ where c is the Zr concentration in the fluid (ppm by weight), T is temperature (K) and ρ is the fluid density (g cm−3). An additional experiment with a saline fluid (15 wt.% NaCl) revealed an increase in zircon solubility by a factor of 3 (4.8 ± 1.6 ppm Zr at 890 °C and 14 kbar) whereas addition of 4.5 wt.% albite as solute increased solubility by about a factor of 5. The Zr solubility at the forsterite–enstatite silica buffer appears to be slightly higher than that at the quartz buffer and it further increases at baddeleyite saturation (48 ± 15 ppm Zr at 930 °C and 16 kbar). These observations are consistent with the stability of zircon relative to ZrO2 + SiO2 and suggest that Zr–Si complexes are not abundant in the fluid. During slab dehydration, the Zr content in the aqueous fluid is predicted to be 1–4 ppm. Mass balance calculations imply that the high field strength element concentrations in primary arc melts will slightly decrease due to the dilution effect of infiltrating fluid. By contrast, mobile lithophile elements are predicted to increase their abundances in the melt by orders of magnitude. Our results suggest that the high abundance of large ion lithophile elements relative to high field strength elements in arc magmas is related to different solubilities of these elements in aqueous fluids migrating from the slab to the magma source regions." @default.
• W2012154227 created "2016-06-24" @default.
• W2012154227 creator A5003588872 @default.
• W2012154227 creator A5031642619 @default.
• W2012154227 creator A5066572736 @default.
• W2012154227 creator A5084913703 @default.
• W2012154227 date "2013-10-01" @default.
• W2012154227 modified "2023-10-04" @default.
• W2012154227 title "Zircon solubility in aqueous fluids at high temperatures and pressures" @default.
• W2012154227 cites W1489332407 @default.
• W2012154227 cites W1566514932 @default.
• W2012154227 cites W1841768873 @default.
• W2012154227 cites W1923294094 @default.
• W2012154227 cites W1969516222 @default.
• W2012154227 cites W1969859799 @default.
• W2012154227 cites W1970207830 @default.
• W2012154227 cites W1970851365 @default.
• W2012154227 cites W1973124747 @default.
• W2012154227 cites W1974156473 @default.
• W2012154227 cites W1986154999 @default.
• W2012154227 cites W1987652319 @default.
• W2012154227 cites W1990633333 @default.
• W2012154227 cites W1991867586 @default.
• W2012154227 cites W1992708421 @default.
• W2012154227 cites W1995378196 @default.
• W2012154227 cites W1999320118 @default.
• W2012154227 cites W2008935602 @default.
• W2012154227 cites W2011221631 @default.
• W2012154227 cites W2011542776 @default.
• W2012154227 cites W2014608018 @default.
• W2012154227 cites W2016675857 @default.
• W2012154227 cites W2018166835 @default.
• W2012154227 cites W2020384898 @default.
• W2012154227 cites W2029850329 @default.
• W2012154227 cites W2031272494 @default.
• W2012154227 cites W2031621767 @default.
• W2012154227 cites W2035283420 @default.
• W2012154227 cites W2036255513 @default.
• W2012154227 cites W2039064764 @default.
• W2012154227 cites W2042731771 @default.
• W2012154227 cites W2046099038 @default.
• W2012154227 cites W2046832831 @default.
• W2012154227 cites W2052594374 @default.
• W2012154227 cites W2054620347 @default.
• W2012154227 cites W2063645155 @default.
• W2012154227 cites W2068182820 @default.
• W2012154227 cites W2068281039 @default.
• W2012154227 cites W2071324209 @default.
• W2012154227 cites W2077191925 @default.
• W2012154227 cites W2077577717 @default.
• W2012154227 cites W2079650581 @default.
• W2012154227 cites W2081315268 @default.
• W2012154227 cites W2087035217 @default.
• W2012154227 cites W2087075409 @default.
• W2012154227 cites W2091624736 @default.
• W2012154227 cites W2094778701 @default.
• W2012154227 cites W2097574848 @default.
• W2012154227 cites W2100841727 @default.
• W2012154227 cites W2114631444 @default.
• W2012154227 cites W2118649177 @default.
• W2012154227 cites W2126929259 @default.
• W2012154227 cites W2129093747 @default.
• W2012154227 cites W2134557517 @default.
• W2012154227 cites W2134953526 @default.
• W2012154227 cites W2138484143 @default.
• W2012154227 cites W2148514253 @default.
• W2012154227 cites W2152681222 @default.
• W2012154227 cites W2154403386 @default.
• W2012154227 cites W2155272764 @default.
• W2012154227 cites W2163762918 @default.
• W2012154227 cites W2167130856 @default.
• W2012154227 cites W2282446225 @default.
• W2012154227 cites W2322101692 @default.
• W2012154227 cites W2342640905 @default.
• W2012154227 cites W2343215739 @default.
• W2012154227 doi "https://doi.org/10.1016/j.gca.2013.05.018" @default.
• W2012154227 hasPublicationYear "2013" @default.
• W2012154227 type Work @default.
• W2012154227 sameAs 2012154227 @default.
• W2012154227 citedByCount "49" @default.
• W2012154227 countsByYear W20121542272014 @default.
• W2012154227 countsByYear W20121542272015 @default.
• W2012154227 countsByYear W20121542272016 @default.
• W2012154227 countsByYear W20121542272017 @default.
• W2012154227 countsByYear W20121542272018 @default.
• W2012154227 countsByYear W20121542272019 @default.
• W2012154227 countsByYear W20121542272020 @default.
• W2012154227 countsByYear W20121542272021 @default.
• W2012154227 countsByYear W20121542272022 @default.
• W2012154227 countsByYear W20121542272023 @default.
• W2012154227 crossrefType "journal-article" @default.
• W2012154227 hasAuthorship W2012154227A5003588872 @default.
• W2012154227 hasAuthorship W2012154227A5031642619 @default.
• W2012154227 hasAuthorship W2012154227A5066572736 @default.
• W2012154227 hasAuthorship W2012154227A5084913703 @default.
• W2012154227 hasConcept C121332964 @default.
• W2012154227 hasConcept C127313418 @default.
• W2012154227 hasConcept C127413603 @default.

• next