Matches in SemOpenAlex for { <https://semopenalex.org/work/W2028476403> ?p ?o ?g. }
- W2028476403 endingPage "147" @default.
- W2028476403 startingPage "128" @default.
- W2028476403 abstract "Dabbahu is a composite volcano at the north end of the active Manda-Hararo segment of the Afar Rift in northern Ethiopia. We present 93 new whole-rock analyses, mineral analyses from 65 samples, and 9 new 40Ar39Ar dates for rocks ranging in composition from mildly alkaline basalt through trachyandesite to peralkaline rhyolite (comendite and pantellerite) erupted from Dabbahu. These data, supplemented by a new geological map, are used to provide insights into the evolution of the volcano. We show that Dabbahu has been active for over 67 k.y., but an apparent hiatus occurred between the eruption of comendite (29 ka) and pantellerite (ca. 8 ka) lavas. Mineral data for olivine, clinopyroxene, plagioclase, and alkali feldspar show a remarkably extensive range of solid solution across the rock suite consistent with protracted fractionation from basalt to rhyolite. The parental basalt is compositionally similar to recent rift-related basalts in the Manda-Hararo rift, with low initial H2O contents (<1 wt%). Closed-system fractionation increased H2O contents of residual liquids sufficiently for some rhyolites to erupt both explosively and effusively. The diverse magma types were erupted from a relatively closely spaced network of vents and fissures. Field evidence indicates that magmas were not erupted in a simple fractionation sequence. Some mixing occurred between magmas of less-evolved compositions and more-evolved compositions shortly prior to, or during, eruption. The differentiation of basalt to rhyolite must have occurred on time scales that were relatively short compared to the lifetime of the volcano, probably due to the small volumes of basalt intruded into the crust and consequently enhanced cooling and crystallization rates. A network of stacked sills or closely spaced dikes in the shallow to midcrust represents the most plausible configuration of the subvolcanic plumbing system. Input of new magma batches into such a system may serve as a key eruption trigger at Dabbahu." @default.
- W2028476403 created "2016-06-24" @default.
- W2028476403 creator A5010468868 @default.
- W2028476403 creator A5068914361 @default.
- W2028476403 creator A5088458520 @default.
- W2028476403 creator A5090222248 @default.
- W2028476403 date "2012-10-25" @default.
- W2028476403 modified "2023-10-02" @default.
- W2028476403 title "Magmatic history of Dabbahu, a composite volcano in the Afar Rift, Ethiopia" @default.
- W2028476403 cites W1533189974 @default.
- W2028476403 cites W1595064302 @default.
- W2028476403 cites W1641367876 @default.
- W2028476403 cites W1966116805 @default.
- W2028476403 cites W1976037363 @default.
- W2028476403 cites W1977568850 @default.
- W2028476403 cites W1981985585 @default.
- W2028476403 cites W1988339658 @default.
- W2028476403 cites W2005781643 @default.
- W2028476403 cites W2006369806 @default.
- W2028476403 cites W2008602349 @default.
- W2028476403 cites W2012411784 @default.
- W2028476403 cites W2012790889 @default.
- W2028476403 cites W2014190886 @default.
- W2028476403 cites W2017688131 @default.
- W2028476403 cites W2020191076 @default.
- W2028476403 cites W2021987309 @default.
- W2028476403 cites W2024664631 @default.
- W2028476403 cites W2028407735 @default.
- W2028476403 cites W2031489692 @default.
- W2028476403 cites W2037588390 @default.
- W2028476403 cites W2039154001 @default.
- W2028476403 cites W2040092205 @default.
- W2028476403 cites W2044886155 @default.
- W2028476403 cites W2047984198 @default.
- W2028476403 cites W2049412643 @default.
- W2028476403 cites W2063992088 @default.
- W2028476403 cites W2074686196 @default.
- W2028476403 cites W2076272192 @default.
- W2028476403 cites W2077028606 @default.
- W2028476403 cites W2078005590 @default.
- W2028476403 cites W2085271975 @default.
- W2028476403 cites W2086179957 @default.
- W2028476403 cites W2091616693 @default.
- W2028476403 cites W2099380715 @default.
- W2028476403 cites W2100979625 @default.
- W2028476403 cites W2110009781 @default.
- W2028476403 cites W2111102974 @default.
- W2028476403 cites W2113519604 @default.
- W2028476403 cites W2117863546 @default.
- W2028476403 cites W2121013006 @default.
- W2028476403 cites W2128475547 @default.
- W2028476403 cites W2129877964 @default.
- W2028476403 cites W2141066354 @default.
- W2028476403 cites W2142886584 @default.
- W2028476403 cites W2144103470 @default.
- W2028476403 cites W2144706707 @default.
- W2028476403 cites W2148592023 @default.
- W2028476403 cites W2149576899 @default.
- W2028476403 cites W2154844266 @default.
- W2028476403 cites W2161009583 @default.
- W2028476403 cites W2162046601 @default.
- W2028476403 cites W2165073556 @default.
- W2028476403 cites W2169099735 @default.
- W2028476403 cites W2269131626 @default.
- W2028476403 cites W2285274212 @default.
- W2028476403 cites W2321981993 @default.
- W2028476403 cites W2328047629 @default.
- W2028476403 cites W2330204384 @default.
- W2028476403 cites W2346949530 @default.
- W2028476403 cites W2355082093 @default.
- W2028476403 cites W2901856977 @default.
- W2028476403 cites W570543625 @default.
- W2028476403 doi "https://doi.org/10.1130/b30560.1" @default.
- W2028476403 hasPublicationYear "2012" @default.
- W2028476403 type Work @default.
- W2028476403 sameAs 2028476403 @default.
- W2028476403 citedByCount "38" @default.
- W2028476403 countsByYear W20284764032013 @default.
- W2028476403 countsByYear W20284764032014 @default.
- W2028476403 countsByYear W20284764032015 @default.
- W2028476403 countsByYear W20284764032016 @default.
- W2028476403 countsByYear W20284764032017 @default.
- W2028476403 countsByYear W20284764032018 @default.
- W2028476403 countsByYear W20284764032019 @default.
- W2028476403 countsByYear W20284764032020 @default.
- W2028476403 countsByYear W20284764032021 @default.
- W2028476403 countsByYear W20284764032022 @default.
- W2028476403 countsByYear W20284764032023 @default.
- W2028476403 crossrefType "journal-article" @default.
- W2028476403 hasAuthorship W2028476403A5010468868 @default.
- W2028476403 hasAuthorship W2028476403A5068914361 @default.
- W2028476403 hasAuthorship W2028476403A5088458520 @default.
- W2028476403 hasAuthorship W2028476403A5090222248 @default.
- W2028476403 hasConcept C120806208 @default.
- W2028476403 hasConcept C127313418 @default.
- W2028476403 hasConcept C151730666 @default.
- W2028476403 hasConcept C165205528 @default.
- W2028476403 hasConcept C17409809 @default.