Matches in SemOpenAlex for { <https://semopenalex.org/work/W1966226304> ?p ?o ?g. }
- W1966226304 endingPage "217" @default.
- W1966226304 startingPage "201" @default.
- W1966226304 abstract "A simple physical model is used to link eruption likelihood in continental regions to the size and shape of the volcanic edifice, as well as to magma density and volatile content. A volcanic edifice acts as a surface load and modifies the stress field in upper crustal levels including the magma chamber. It affects the critical magma overpressure for reservoir failure as well as the conditions of dyke ascent from reservoir to surface. Calculations are made for dyke ascent in the stress field due to an overpressured reservoir beneath an edifice. Different edifice shapes are investigated, from shield volcanoes with gentle slopes to stratovolcanoes with steeper flanks. Beneath a mature volcanic edifice, magmatic overpressures required for reservoir failure are large, but not large enough for a dyke to reach the central vent area at the summit. Thus, basaltic summit eruptions can only occur if the amount of dissolved volatiles exceeds some threshold value which increases with edifice size, and hence must be in explosive regimes unless magma is able to degas at shallow depths. For mature volcanic systems, edifice collapse or destruction may lead to renewed basaltic activity through the central vent area." @default.
- W1966226304 created "2016-06-24" @default.
- W1966226304 creator A5006500638 @default.
- W1966226304 creator A5085780751 @default.
- W1966226304 date "2004-09-01" @default.
- W1966226304 modified "2023-10-18" @default.
- W1966226304 title "Likelihood of basaltic eruptions as a function of volatile content and volcanic edifice size" @default.
- W1966226304 cites W192043380 @default.
- W1966226304 cites W1964279737 @default.
- W1966226304 cites W1964965476 @default.
- W1966226304 cites W1966364287 @default.
- W1966226304 cites W1968870983 @default.
- W1966226304 cites W1976132681 @default.
- W1966226304 cites W1978505296 @default.
- W1966226304 cites W1982059564 @default.
- W1966226304 cites W1989288655 @default.
- W1966226304 cites W2008602349 @default.
- W1966226304 cites W2016713956 @default.
- W1966226304 cites W2017853565 @default.
- W1966226304 cites W2021548793 @default.
- W1966226304 cites W2021767154 @default.
- W1966226304 cites W2030100752 @default.
- W1966226304 cites W2030422267 @default.
- W1966226304 cites W2033927110 @default.
- W1966226304 cites W2041007941 @default.
- W1966226304 cites W2045764565 @default.
- W1966226304 cites W2049219813 @default.
- W1966226304 cites W2057613181 @default.
- W1966226304 cites W2071053567 @default.
- W1966226304 cites W2072507292 @default.
- W1966226304 cites W2074636783 @default.
- W1966226304 cites W2078875698 @default.
- W1966226304 cites W2081830829 @default.
- W1966226304 cites W2081910176 @default.
- W1966226304 cites W2093244578 @default.
- W1966226304 cites W2094561109 @default.
- W1966226304 cites W2101045622 @default.
- W1966226304 cites W2123803462 @default.
- W1966226304 cites W2143738823 @default.
- W1966226304 cites W2151626434 @default.
- W1966226304 cites W2155715600 @default.
- W1966226304 cites W2159437069 @default.
- W1966226304 cites W2165281724 @default.
- W1966226304 cites W2170333136 @default.
- W1966226304 cites W2319531913 @default.
- W1966226304 doi "https://doi.org/10.1016/j.jvolgeores.2004.05.010" @default.
- W1966226304 hasPublicationYear "2004" @default.
- W1966226304 type Work @default.
- W1966226304 sameAs 1966226304 @default.
- W1966226304 citedByCount "23" @default.
- W1966226304 countsByYear W19662263042012 @default.
- W1966226304 countsByYear W19662263042013 @default.
- W1966226304 countsByYear W19662263042014 @default.
- W1966226304 countsByYear W19662263042018 @default.
- W1966226304 countsByYear W19662263042019 @default.
- W1966226304 countsByYear W19662263042021 @default.
- W1966226304 crossrefType "journal-article" @default.
- W1966226304 hasAuthorship W1966226304A5006500638 @default.
- W1966226304 hasAuthorship W1966226304A5085780751 @default.
- W1966226304 hasConcept C120806208 @default.
- W1966226304 hasConcept C121332964 @default.
- W1966226304 hasConcept C127313418 @default.
- W1966226304 hasConcept C146348940 @default.
- W1966226304 hasConcept C161509811 @default.
- W1966226304 hasConcept C17409809 @default.
- W1966226304 hasConcept C183222429 @default.
- W1966226304 hasConcept C192241223 @default.
- W1966226304 hasConcept C29452850 @default.
- W1966226304 hasConcept C52543455 @default.
- W1966226304 hasConcept C5900021 @default.
- W1966226304 hasConcept C75946609 @default.
- W1966226304 hasConcept C9566828 @default.
- W1966226304 hasConcept C97355855 @default.
- W1966226304 hasConceptScore W1966226304C120806208 @default.
- W1966226304 hasConceptScore W1966226304C121332964 @default.
- W1966226304 hasConceptScore W1966226304C127313418 @default.
- W1966226304 hasConceptScore W1966226304C146348940 @default.
- W1966226304 hasConceptScore W1966226304C161509811 @default.
- W1966226304 hasConceptScore W1966226304C17409809 @default.
- W1966226304 hasConceptScore W1966226304C183222429 @default.
- W1966226304 hasConceptScore W1966226304C192241223 @default.
- W1966226304 hasConceptScore W1966226304C29452850 @default.
- W1966226304 hasConceptScore W1966226304C52543455 @default.
- W1966226304 hasConceptScore W1966226304C5900021 @default.
- W1966226304 hasConceptScore W1966226304C75946609 @default.
- W1966226304 hasConceptScore W1966226304C9566828 @default.
- W1966226304 hasConceptScore W1966226304C97355855 @default.
- W1966226304 hasIssue "1-3" @default.
- W1966226304 hasLocation W19662263041 @default.
- W1966226304 hasOpenAccess W1966226304 @default.
- W1966226304 hasPrimaryLocation W19662263041 @default.
- W1966226304 hasRelatedWork W1535068549 @default.
- W1966226304 hasRelatedWork W1964880660 @default.
- W1966226304 hasRelatedWork W1966226304 @default.
- W1966226304 hasRelatedWork W2019718787 @default.
- W1966226304 hasRelatedWork W2057817903 @default.
- W1966226304 hasRelatedWork W2086564367 @default.
- W1966226304 hasRelatedWork W2098333284 @default.