FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2270291524> ?p ?o ?g. }

• W2270291524 endingPage "287" @default.
• W2270291524 startingPage "272" @default.
• W2270291524 abstract "The elemental and isotopic compositions of noble gases (He, Ne, and Ar) in olivine- and clinopyroxene-hosted fluid inclusions have been measured for rocks at various degrees of evolution and belonging to high-K calcalkaline–shoshonitic and shoshonitic–potassic series in order to cover the entire volcanological history of Vulcano Island (Italy). The major- and trace-element concentrations and the Sr- and Pb-isotope compositions for whole rocks were integrated with data obtained from the fluid inclusions. 3He/4He in fluid inclusions is within the range of 3.30 and 5.94 R/Ra, being lower than the theoretical value for the deep magmatic source expected for Vulcano Island (6.0–6.2 R/Ra). 3He/4He of the magmatic source is almost constant throughout the volcanic history of Vulcano. Integration of the He- and Sr-isotope systematics leads to the conclusion that a decrease in the He-isotope ratio of the rocks is mainly due to the assimilation of 10–25% of a crustal component similar to the Calabrian basement. 3He/4He shows a negative correlation with Sr isotopes except for the last-erupted Vulcanello latites (Punta del Roveto), which have anomalously high He isotope ratios. This anomaly has been attributed to a flushing process by fluids coming from the deepest reservoirs, since an input of deep magmatic volatiles with high 3He/4He values increases the He-isotope ratio without changing 87Sr/86Sr. A comparison of the He-isotope ratios between fluid inclusions and fumarolic gases shows that only the basalts of La Sommata and the latites of Vulcanello have comparable values. Taking into account that the latites of Vulcanello relate to one of the most-recent eruptions at Vulcano (in the 17th century), we infer that the most probable magma which actually feeds the fumarolic emissions is a latitic body that ponded at about 3–3.5 km of depth and is flushed by fluids coming from a deeper and basic magma." @default.
• W2270291524 created "2016-06-24" @default.
• W2270291524 creator A5024279292 @default.
• W2270291524 creator A5027998868 @default.
• W2270291524 creator A5046242967 @default.
• W2270291524 creator A5054407796 @default.
• W2270291524 creator A5063376609 @default.
• W2270291524 creator A5078961744 @default.
• W2270291524 date "2016-04-01" @default.
• W2270291524 modified "2023-10-16" @default.
• W2270291524 title "Revealing magma degassing below closed-conduit active volcanoes: Geochemical features of volcanic rocks versus fumarolic fluids at Vulcano (Aeolian Islands, Italy)" @default.
• W2270291524 cites W1542915903 @default.
• W2270291524 cites W1585397976 @default.
• W2270291524 cites W1825299619 @default.
• W2270291524 cites W1965082042 @default.
• W2270291524 cites W1965923240 @default.
• W2270291524 cites W1967261063 @default.
• W2270291524 cites W1969859799 @default.
• W2270291524 cites W1970963438 @default.
• W2270291524 cites W1973438572 @default.
• W2270291524 cites W1978715234 @default.
• W2270291524 cites W1981971984 @default.
• W2270291524 cites W1983227122 @default.
• W2270291524 cites W2002473398 @default.
• W2270291524 cites W2002700339 @default.
• W2270291524 cites W2005123230 @default.
• W2270291524 cites W2007359145 @default.
• W2270291524 cites W2008136270 @default.
• W2270291524 cites W2013207924 @default.
• W2270291524 cites W2014978996 @default.
• W2270291524 cites W2016269017 @default.
• W2270291524 cites W2017933163 @default.
• W2270291524 cites W2019622868 @default.
• W2270291524 cites W2021134687 @default.
• W2270291524 cites W2021566798 @default.
• W2270291524 cites W2021925896 @default.
• W2270291524 cites W2022939468 @default.
• W2270291524 cites W2024784417 @default.
• W2270291524 cites W2026701476 @default.
• W2270291524 cites W2030387090 @default.
• W2270291524 cites W2032960086 @default.
• W2270291524 cites W2036993022 @default.
• W2270291524 cites W2037654520 @default.
• W2270291524 cites W2038120078 @default.
• W2270291524 cites W2043589082 @default.
• W2270291524 cites W2045212032 @default.
• W2270291524 cites W2046459929 @default.
• W2270291524 cites W2047911230 @default.
• W2270291524 cites W2049819144 @default.
• W2270291524 cites W2052837700 @default.
• W2270291524 cites W2053099553 @default.
• W2270291524 cites W2063177053 @default.
• W2270291524 cites W2063307255 @default.
• W2270291524 cites W2073321433 @default.
• W2270291524 cites W2074884435 @default.
• W2270291524 cites W2077181789 @default.
• W2270291524 cites W2078042171 @default.
• W2270291524 cites W2078376125 @default.
• W2270291524 cites W2078840355 @default.
• W2270291524 cites W2079765725 @default.
• W2270291524 cites W2080590712 @default.
• W2270291524 cites W2082192617 @default.
• W2270291524 cites W2084338653 @default.
• W2270291524 cites W2085464211 @default.
• W2270291524 cites W2089502158 @default.
• W2270291524 cites W2090258675 @default.
• W2270291524 cites W2094580500 @default.
• W2270291524 cites W2105931551 @default.
• W2270291524 cites W2108548522 @default.
• W2270291524 cites W2112737386 @default.
• W2270291524 cites W2122921215 @default.
• W2270291524 cites W2128840812 @default.
• W2270291524 cites W2145878461 @default.
• W2270291524 cites W2156339013 @default.
• W2270291524 cites W2159745880 @default.
• W2270291524 cites W2171737369 @default.
• W2270291524 cites W2605589018 @default.
• W2270291524 doi "https://doi.org/10.1016/j.lithos.2016.01.026" @default.
• W2270291524 hasPublicationYear "2016" @default.
• W2270291524 type Work @default.
• W2270291524 sameAs 2270291524 @default.
• W2270291524 citedByCount "29" @default.
• W2270291524 countsByYear W22702915242017 @default.
• W2270291524 countsByYear W22702915242018 @default.
• W2270291524 countsByYear W22702915242019 @default.
• W2270291524 countsByYear W22702915242020 @default.
• W2270291524 countsByYear W22702915242021 @default.
• W2270291524 countsByYear W22702915242022 @default.
• W2270291524 countsByYear W22702915242023 @default.
• W2270291524 crossrefType "journal-article" @default.
• W2270291524 hasAuthorship W2270291524A5024279292 @default.
• W2270291524 hasAuthorship W2270291524A5027998868 @default.
• W2270291524 hasAuthorship W2270291524A5046242967 @default.
• W2270291524 hasAuthorship W2270291524A5054407796 @default.
• W2270291524 hasAuthorship W2270291524A5063376609 @default.
• W2270291524 hasAuthorship W2270291524A5078961744 @default.
• W2270291524 hasConcept C120806208 @default.
• W2270291524 hasConcept C121332964 @default.

• next