FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2120747481> ?p ?o ?g. }

• W2120747481 endingPage "1047" @default.
• W2120747481 startingPage "1029" @default.
• W2120747481 abstract "The Izu–Bonin volcanic arc is an excellent example of an intra-oceanic convergent margin. A total of 1011 chemical analyses of 17 Quaternary volcanoes of the arc are reviewed to estimate relative proportions of magmas erupted. Basalt and basic andesite (SiO2 < 57 wt %) are the predominant eruptive products of the Izu–Bonin arc, and rhyolite (SiO2 > 70 wt %) forms another peak in volume. Such rhyolites possess compositions identical to those of partial melts produced by dehydration-melting of calc-alkaline andesites at low pressure (<7 kbar). Meanwhile, the major element variation of the Shirahama Group Mio-Pliocene volcanic arc suite, Izu Peninsula, completely overlaps that of the Quaternary Izu–Bonin arc volcanoes, and groundmasses of Shirahama Group calc-alkaline andesites have compositions similar to those of Izu–Bonin rhyolites. Moreover, phenocryst assemblages of calc-alkaline andesites of the Shirahama Group resemble restite phase assemblages of dehydration-melting of calc-alkaline andesite. These lines of evidence suggest that the rhyolite magmas may have been produced by dehydration-melting of calc-alkaline andesite in the upper to middle crust. If so, then the presence of large amounts of calc-alkaline andesite (3–5 times more abundant than the rhyolites) within the oceanic arc crust would be expected, which is consistent with a recently proposed structural model across the Izu–Bonin arc. The calc-alkaline andesite magmas may be water saturated, and would crystallize extensively and solidify within the crust. The model proposed here suggests that rhyolite eruptions could be triggered by an influx of hot basalt magma from depth, reheating and partially melting the calc-alkaline andesite component of the crust." @default.
• W2120747481 created "2016-06-24" @default.
• W2120747481 creator A5023787504 @default.
• W2120747481 date "2002-06-01" @default.
• W2120747481 modified "2023-10-17" @default.
• W2120747481 title "Remelting of an Andesitic Crust as a Possible Origin for Rhyolitic Magma in Oceanic Arcs: an Example from the Izu-Bonin Arc" @default.
• W2120747481 cites W1981756317 @default.
• W2120747481 cites W1991848112 @default.
• W2120747481 cites W1994300579 @default.
• W2120747481 cites W2008782416 @default.
• W2120747481 cites W2009618656 @default.
• W2120747481 cites W2013340586 @default.
• W2120747481 cites W2016548466 @default.
• W2120747481 cites W2025307763 @default.
• W2120747481 cites W2029413472 @default.
• W2120747481 cites W2029867360 @default.
• W2120747481 cites W2037582288 @default.
• W2120747481 cites W2043694977 @default.
• W2120747481 cites W2047541285 @default.
• W2120747481 cites W2053499757 @default.
• W2120747481 cites W2065112342 @default.
• W2120747481 cites W2072117420 @default.
• W2120747481 cites W2078562202 @default.
• W2120747481 cites W2079376467 @default.
• W2120747481 cites W2079748421 @default.
• W2120747481 cites W2081684341 @default.
• W2120747481 cites W2092692526 @default.
• W2120747481 cites W2092720835 @default.
• W2120747481 cites W2096853082 @default.
• W2120747481 cites W2103549174 @default.
• W2120747481 cites W2106625794 @default.
• W2120747481 cites W2114118704 @default.
• W2120747481 cites W2149354811 @default.
• W2120747481 cites W2158458004 @default.
• W2120747481 cites W2181479233 @default.
• W2120747481 cites W2184612481 @default.
• W2120747481 cites W2186364880 @default.
• W2120747481 cites W2256566153 @default.
• W2120747481 cites W2303806580 @default.
• W2120747481 cites W2313102481 @default.
• W2120747481 cites W2325019720 @default.
• W2120747481 cites W2334581221 @default.
• W2120747481 cites W2469646072 @default.
• W2120747481 cites W2490037028 @default.
• W2120747481 cites W2497862200 @default.
• W2120747481 cites W2506090427 @default.
• W2120747481 cites W2510021459 @default.
• W2120747481 cites W2571188112 @default.
• W2120747481 cites W2588221747 @default.
• W2120747481 cites W2900747449 @default.
• W2120747481 cites W3001181352 @default.
• W2120747481 cites W3017375622 @default.
• W2120747481 cites W3136689746 @default.
• W2120747481 cites W3197760842 @default.
• W2120747481 cites W611272396 @default.
• W2120747481 cites W2505011468 @default.
• W2120747481 doi "https://doi.org/10.1093/petrology/43.6.1029" @default.
• W2120747481 hasPublicationYear "2002" @default.
• W2120747481 type Work @default.
• W2120747481 sameAs 2120747481 @default.
• W2120747481 citedByCount "213" @default.
• W2120747481 countsByYear W21207474812012 @default.
• W2120747481 countsByYear W21207474812013 @default.
• W2120747481 countsByYear W21207474812014 @default.
• W2120747481 countsByYear W21207474812015 @default.
• W2120747481 countsByYear W21207474812016 @default.
• W2120747481 countsByYear W21207474812017 @default.
• W2120747481 countsByYear W21207474812018 @default.
• W2120747481 countsByYear W21207474812019 @default.
• W2120747481 countsByYear W21207474812020 @default.
• W2120747481 countsByYear W21207474812021 @default.
• W2120747481 countsByYear W21207474812022 @default.
• W2120747481 countsByYear W21207474812023 @default.
• W2120747481 crossrefType "journal-article" @default.
• W2120747481 hasAuthorship W2120747481A5023787504 @default.
• W2120747481 hasBestOaLocation W21207474811 @default.
• W2120747481 hasConcept C120806208 @default.
• W2120747481 hasConcept C127313418 @default.
• W2120747481 hasConcept C151730666 @default.
• W2120747481 hasConcept C161509811 @default.
• W2120747481 hasConcept C17409809 @default.
• W2120747481 hasConcept C180492444 @default.
• W2120747481 hasConcept C183222429 @default.
• W2120747481 hasConcept C192241223 @default.
• W2120747481 hasConcept C25822816 @default.
• W2120747481 hasConcept C2776698055 @default.
• W2120747481 hasConcept C2779321686 @default.
• W2120747481 hasConcept C2781323139 @default.
• W2120747481 hasConcept C36986328 @default.
• W2120747481 hasConcept C49708893 @default.
• W2120747481 hasConcept C58097730 @default.
• W2120747481 hasConcept C5900021 @default.
• W2120747481 hasConcept C63379926 @default.
• W2120747481 hasConcept C77928131 @default.
• W2120747481 hasConceptScore W2120747481C120806208 @default.
• W2120747481 hasConceptScore W2120747481C127313418 @default.
• W2120747481 hasConceptScore W2120747481C151730666 @default.
• W2120747481 hasConceptScore W2120747481C161509811 @default.

• next