Matches in SemOpenAlex for { <https://semopenalex.org/work/W2152376178> ?p ?o ?g. }
- W2152376178 endingPage "935" @default.
- W2152376178 startingPage "911" @default.
- W2152376178 abstract "Crystallization experiments at 400 MPa, oxidized condition (ΔlogfO2 = NNO + 1, where NNO is nickel–nickel oxide buffer) and over a range of temperatures (850–950°C) and fluid composition (XH2Oin = 0·3–1) have been carried out to constrain the storage conditions of the sulphur-rich magma of the Huerto Andesite (an anhydrite, pyrrhotite, and S-rich apatite-bearing, post-Fish Canyon Tuff mafic lava). The results are used to evaluate the role of fluids released from the crystallization of magmas such as the Huerto Andesite on the remobilization of the largely crystallized dacitic Fish Canyon magma body. Experiments were performed using the natural andesitic bulk composition with and without added sulphur. The presence of sulphur slightly affects the phase equilibria by changing the phase proportions, stability fields of plagioclase, pyroxenes and ilmenite, and also affects the plagioclase composition. Phase equilibria and mineral composition data indicate that the magma may have contained 4·5 wt % water in the melt and that the pre-eruptive temperature was 875 ± 25°C. Assuming that the magma was in equilibrium with a fluid phase, the CO2 concentration of the melt is estimated to be in the range 2000–4000 ppm (at 400 MPa). Before eruption, the andesite had an oxidation state very close to, or slightly within, the co-stability field of anhydrite–pyrrhotite at NNO + 1·1. At these conditions, the sulphur content in the melt is ∼500 ppm. Assuming open-system degassing resulting from continuing crystallization at depth, most of the CO2 dissolved in the andesitic melt should be released after the crystallization of <10 vol. % of the magma, corresponding to a cooling from 875 to 825–850°C. Thus, the fluids released owing to crystallization processes should be mainly composed of water at temperatures below 825°C." @default.
- W2152376178 created "2016-06-24" @default.
- W2152376178 creator A5010094346 @default.
- W2152376178 creator A5026160652 @default.
- W2152376178 creator A5052189114 @default.
- W2152376178 date "2008-03-24" @default.
- W2152376178 modified "2023-09-24" @default.
- W2152376178 title "Pre-eruptive Conditions of the Huerto Andesite (Fish Canyon System, San Juan Volcanic Field, Colorado): Influence of Volatiles (C-O-H-S) on Phase Equilibria and Mineral Composition" @default.
- W2152376178 cites W1540979450 @default.
- W2152376178 cites W1864360925 @default.
- W2152376178 cites W1875889981 @default.
- W2152376178 cites W1955833725 @default.
- W2152376178 cites W1967277465 @default.
- W2152376178 cites W1968389139 @default.
- W2152376178 cites W1972828185 @default.
- W2152376178 cites W1982630226 @default.
- W2152376178 cites W1983219147 @default.
- W2152376178 cites W1988457006 @default.
- W2152376178 cites W2009717233 @default.
- W2152376178 cites W2018877747 @default.
- W2152376178 cites W2035041137 @default.
- W2152376178 cites W2036368107 @default.
- W2152376178 cites W2037639782 @default.
- W2152376178 cites W2040120198 @default.
- W2152376178 cites W2043760612 @default.
- W2152376178 cites W2043854317 @default.
- W2152376178 cites W2044816232 @default.
- W2152376178 cites W2053071492 @default.
- W2152376178 cites W2053483240 @default.
- W2152376178 cites W2054481657 @default.
- W2152376178 cites W2054940051 @default.
- W2152376178 cites W2055476712 @default.
- W2152376178 cites W2055595543 @default.
- W2152376178 cites W2059283697 @default.
- W2152376178 cites W2060588282 @default.
- W2152376178 cites W2063449686 @default.
- W2152376178 cites W2063505294 @default.
- W2152376178 cites W2063583381 @default.
- W2152376178 cites W2066999888 @default.
- W2152376178 cites W2074745063 @default.
- W2152376178 cites W2081723971 @default.
- W2152376178 cites W2087025316 @default.
- W2152376178 cites W2094373534 @default.
- W2152376178 cites W2097545423 @default.
- W2152376178 cites W2099401875 @default.
- W2152376178 cites W2099709957 @default.
- W2152376178 cites W2101045622 @default.
- W2152376178 cites W2127236625 @default.
- W2152376178 cites W2127408677 @default.
- W2152376178 cites W2127671904 @default.
- W2152376178 cites W2130612399 @default.
- W2152376178 cites W2142062379 @default.
- W2152376178 cites W2154779351 @default.
- W2152376178 cites W2157508130 @default.
- W2152376178 cites W2159549048 @default.
- W2152376178 cites W2166916464 @default.
- W2152376178 cites W221071987 @default.
- W2152376178 cites W2246871654 @default.
- W2152376178 cites W2291967731 @default.
- W2152376178 cites W2313729992 @default.
- W2152376178 cites W2315205965 @default.
- W2152376178 cites W2330204384 @default.
- W2152376178 cites W2334605366 @default.
- W2152376178 cites W2337815084 @default.
- W2152376178 cites W2341396161 @default.
- W2152376178 cites W2389701078 @default.
- W2152376178 cites W2517397417 @default.
- W2152376178 cites W2556513839 @default.
- W2152376178 cites W2561991964 @default.
- W2152376178 cites W2966351755 @default.
- W2152376178 doi "https://doi.org/10.1093/petrology/egn011" @default.
- W2152376178 hasPublicationYear "2008" @default.
- W2152376178 type Work @default.
- W2152376178 sameAs 2152376178 @default.
- W2152376178 citedByCount "52" @default.
- W2152376178 countsByYear W21523761782012 @default.
- W2152376178 countsByYear W21523761782013 @default.
- W2152376178 countsByYear W21523761782014 @default.
- W2152376178 countsByYear W21523761782015 @default.
- W2152376178 countsByYear W21523761782016 @default.
- W2152376178 countsByYear W21523761782017 @default.
- W2152376178 countsByYear W21523761782018 @default.
- W2152376178 countsByYear W21523761782019 @default.
- W2152376178 countsByYear W21523761782020 @default.
- W2152376178 countsByYear W21523761782021 @default.
- W2152376178 countsByYear W21523761782022 @default.
- W2152376178 countsByYear W21523761782023 @default.
- W2152376178 crossrefType "journal-article" @default.
- W2152376178 hasAuthorship W2152376178A5010094346 @default.
- W2152376178 hasAuthorship W2152376178A5026160652 @default.
- W2152376178 hasAuthorship W2152376178A5052189114 @default.
- W2152376178 hasConcept C114793014 @default.
- W2152376178 hasConcept C120806208 @default.
- W2152376178 hasConcept C127313418 @default.
- W2152376178 hasConcept C138885662 @default.
- W2152376178 hasConcept C17409809 @default.
- W2152376178 hasConcept C178790620 @default.
- W2152376178 hasConcept C185592680 @default.