FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2087616905> ?p ?o ?g. }

• W2087616905 endingPage "74" @default.
• W2087616905 startingPage "57" @default.
• W2087616905 abstract "Abstract This study reports and discusses a set of new K/Ar age and new petrochemical data on basalts of the Jabal Eghei (Nuqay) area (south Libya). This area is part of a > 1000 km long NNW–SSE Libyan volcanic field that stretches from the Mediterranean coastal near Tripoli to the Tibesti massif in Chad. Whole rock K/Ar ages, stratigraphy, volcanology and rock petrochemistry indicate that the Jabal Eghei developed during two volcanic events. The first occurred from the Middle Miocene to the Pliocene (K/Ar ages from ~ 16 to ~ 5 Ma) when large volumes of low aspect ratio lava flows of transitional basalts formed. The second event happened in Pliocene–mid-Pleistocene time (4–≤ 1 Ma) and it gave rise to basanite spatter to scoria pyroclastic cones and subordinate lava flow facies. The transitional basalts are less primitive and less enriched in incompatible trace elements than the basanites. Petrochemical characteristics reveal that the transitional basalts underwent weak to moderate olivine-dominated fractionation and that crustal assimilation had negligible effects. REE geochemical modeling shows that primary magmas of both transitional basalts and basanites formed by melting of a similar garnet-bearing, primitive mantle-like source with degree of melting of 3–5% and ≤ 1%, respectively. It is also demonstrated that the transitional basalts show systematic compositional changes in time because progressively younger rocks are petrochemically more similar to basanites. We argue that our data definitely prove that the age pattern along the entire Libyan volcanic field is much more complex than it was thought before." @default.
• W2087616905 created "2016-06-24" @default.
• W2087616905 creator A5009614621 @default.
• W2087616905 creator A5031854169 @default.
• W2087616905 creator A5045797678 @default.
• W2087616905 creator A5052854967 @default.
• W2087616905 creator A5061577853 @default.
• W2087616905 creator A5063176117 @default.
• W2087616905 date "2015-02-01" @default.
• W2087616905 modified "2023-10-11" @default.
• W2087616905 title "Neogene to Quaternary basalts of the Jabal Eghei (Nuqay) area (south Libya): Two distinct volcanic events or continuous volcanism with gradual shift in magma composition?" @default.
• W2087616905 cites W1485237895 @default.
• W2087616905 cites W1588350386 @default.
• W2087616905 cites W1623582059 @default.
• W2087616905 cites W1914890451 @default.
• W2087616905 cites W1969385291 @default.
• W2087616905 cites W1969859799 @default.
• W2087616905 cites W1972863953 @default.
• W2087616905 cites W1973582422 @default.
• W2087616905 cites W1974075351 @default.
• W2087616905 cites W1974731988 @default.
• W2087616905 cites W1978658483 @default.
• W2087616905 cites W1980544584 @default.
• W2087616905 cites W1982987959 @default.
• W2087616905 cites W1983365083 @default.
• W2087616905 cites W1984179600 @default.
• W2087616905 cites W1985957692 @default.
• W2087616905 cites W1986714390 @default.
• W2087616905 cites W1987907556 @default.
• W2087616905 cites W1988369251 @default.
• W2087616905 cites W1988430460 @default.
• W2087616905 cites W1990740187 @default.
• W2087616905 cites W1991167114 @default.
• W2087616905 cites W2007730638 @default.
• W2087616905 cites W2009544440 @default.
• W2087616905 cites W2010771702 @default.
• W2087616905 cites W2012397486 @default.
• W2087616905 cites W2013281812 @default.
• W2087616905 cites W2021987309 @default.
• W2087616905 cites W2022060797 @default.
• W2087616905 cites W2022648729 @default.
• W2087616905 cites W2026379820 @default.
• W2087616905 cites W2027862110 @default.
• W2087616905 cites W2035044185 @default.
• W2087616905 cites W2035642076 @default.
• W2087616905 cites W2037546356 @default.
• W2087616905 cites W2041193569 @default.
• W2087616905 cites W2042692134 @default.
• W2087616905 cites W2044349646 @default.
• W2087616905 cites W2045356160 @default.
• W2087616905 cites W2055812626 @default.
• W2087616905 cites W2059585335 @default.
• W2087616905 cites W2060559823 @default.
• W2087616905 cites W2064568067 @default.
• W2087616905 cites W2067703344 @default.
• W2087616905 cites W2067997488 @default.
• W2087616905 cites W2068132275 @default.
• W2087616905 cites W2068698418 @default.
• W2087616905 cites W2072003048 @default.
• W2087616905 cites W2072105912 @default.
• W2087616905 cites W2072128807 @default.
• W2087616905 cites W2075031757 @default.
• W2087616905 cites W2076388142 @default.
• W2087616905 cites W2076625969 @default.
• W2087616905 cites W2076755830 @default.
• W2087616905 cites W2079855816 @default.
• W2087616905 cites W2090570612 @default.
• W2087616905 cites W2115532364 @default.
• W2087616905 cites W2137427519 @default.
• W2087616905 cites W2143863579 @default.
• W2087616905 cites W2145604970 @default.
• W2087616905 cites W2151154332 @default.
• W2087616905 cites W2161724824 @default.
• W2087616905 cites W2166978438 @default.
• W2087616905 cites W2171246880 @default.
• W2087616905 cites W4247433290 @default.
• W2087616905 cites W4322389022 @default.
• W2087616905 doi "https://doi.org/10.1016/j.jvolgeores.2015.02.003" @default.
• W2087616905 hasPublicationYear "2015" @default.
• W2087616905 type Work @default.
• W2087616905 sameAs 2087616905 @default.
• W2087616905 citedByCount "11" @default.
• W2087616905 countsByYear W20876169052016 @default.
• W2087616905 countsByYear W20876169052017 @default.
• W2087616905 countsByYear W20876169052018 @default.
• W2087616905 countsByYear W20876169052019 @default.
• W2087616905 countsByYear W20876169052020 @default.
• W2087616905 countsByYear W20876169052021 @default.
• W2087616905 crossrefType "journal-article" @default.
• W2087616905 hasAuthorship W2087616905A5009614621 @default.
• W2087616905 hasAuthorship W2087616905A5031854169 @default.
• W2087616905 hasAuthorship W2087616905A5045797678 @default.
• W2087616905 hasAuthorship W2087616905A5052854967 @default.
• W2087616905 hasAuthorship W2087616905A5061577853 @default.
• W2087616905 hasAuthorship W2087616905A5063176117 @default.
• W2087616905 hasConcept C109007969 @default.
• W2087616905 hasConcept C120806208 @default.
• W2087616905 hasConcept C127313418 @default.

• next