Matches in SemOpenAlex for { <https://semopenalex.org/work/W2105169341> ?p ?o ?g. }
Showing items 1 to 76 of
76
with 100 items per page.
- W2105169341 endingPage "377" @default.
- W2105169341 startingPage "361" @default.
- W2105169341 abstract "The palaeontologically dated Ordovician associations of the Peloritan Mountains consist of metasilts, metapelites, calc-schists and metavolcanic rocks. These rocks form a portion of a terrigenous-volcanic-carbonate sequence of Cambro-Ordovician to Carboniferous age. This Palaeozoic sequence occupies the lower tectonic position in a Variscan orogen, affected by later Alpine deformation. The upper portion of this orogen is formed by low to high grade metamorphic rocks and some rare magmatic rocks. The Ordovician section of the sequence is divisible into a lower part (probably Arenigian), characterized by frequent and extensive within-plate alkaline metabasalts, and an upper part characterized by metadacites and metarhyolites intercalated with metasediments, commonly carbonates. The chemical characteristics of the metavolcanic rocks and the composition and structure of the metasediments indicate the persistence of tensional conditions during the Lower Ordovician. In contrast, the Upper Ordovician was marked by reducing tension, stagnation of basaltic magmas at different crustal levels, and consequent formation of dacitic and rhyolitic melts by partial melting of the surrounding crust. A comparison of the Ordovician sequences of the Peloritan Mountains with those of the Calabrian Palaeozoic basins shows several geodynamic similarities. Among other circum-Mediterranean basins, only that of north-western Bulgaria shows good analogies." @default.
- W2105169341 created "2016-06-24" @default.
- W2105169341 creator A5059646207 @default.
- W2105169341 creator A5061819642 @default.
- W2105169341 creator A5071572398 @default.
- W2105169341 date "1992-10-01" @default.
- W2105169341 modified "2023-09-25" @default.
- W2105169341 title "Ordovician volcanism of the Peloritan Mountains (Sicily): Implications for evolution of Palaeozoic basins in the Calabrian-Peloritan Arc" @default.
- W2105169341 cites W1966934203 @default.
- W2105169341 cites W1986760631 @default.
- W2105169341 cites W2000536741 @default.
- W2105169341 cites W2008783408 @default.
- W2105169341 cites W2018910343 @default.
- W2105169341 cites W2035597521 @default.
- W2105169341 cites W2054933791 @default.
- W2105169341 cites W2056232757 @default.
- W2105169341 cites W2080214030 @default.
- W2105169341 cites W2089502158 @default.
- W2105169341 cites W2108971421 @default.
- W2105169341 cites W2132896830 @default.
- W2105169341 cites W2145191782 @default.
- W2105169341 cites W2151802570 @default.
- W2105169341 cites W3091773740 @default.
- W2105169341 doi "https://doi.org/10.1002/gj.3350270406" @default.
- W2105169341 hasPublicationYear "1992" @default.
- W2105169341 type Work @default.
- W2105169341 sameAs 2105169341 @default.
- W2105169341 citedByCount "3" @default.
- W2105169341 countsByYear W21051693412018 @default.
- W2105169341 crossrefType "journal-article" @default.
- W2105169341 hasAuthorship W2105169341A5059646207 @default.
- W2105169341 hasAuthorship W2105169341A5061819642 @default.
- W2105169341 hasAuthorship W2105169341A5071572398 @default.
- W2105169341 hasConcept C109007969 @default.
- W2105169341 hasConcept C120806208 @default.
- W2105169341 hasConcept C127313418 @default.
- W2105169341 hasConcept C13106087 @default.
- W2105169341 hasConcept C149918038 @default.
- W2105169341 hasConcept C151730666 @default.
- W2105169341 hasConcept C161509811 @default.
- W2105169341 hasConcept C17409809 @default.
- W2105169341 hasConcept C192241223 @default.
- W2105169341 hasConcept C25822816 @default.
- W2105169341 hasConcept C91442348 @default.
- W2105169341 hasConceptScore W2105169341C109007969 @default.
- W2105169341 hasConceptScore W2105169341C120806208 @default.
- W2105169341 hasConceptScore W2105169341C127313418 @default.
- W2105169341 hasConceptScore W2105169341C13106087 @default.
- W2105169341 hasConceptScore W2105169341C149918038 @default.
- W2105169341 hasConceptScore W2105169341C151730666 @default.
- W2105169341 hasConceptScore W2105169341C161509811 @default.
- W2105169341 hasConceptScore W2105169341C17409809 @default.
- W2105169341 hasConceptScore W2105169341C192241223 @default.
- W2105169341 hasConceptScore W2105169341C25822816 @default.
- W2105169341 hasConceptScore W2105169341C91442348 @default.
- W2105169341 hasIssue "4" @default.
- W2105169341 hasLocation W21051693411 @default.
- W2105169341 hasOpenAccess W2105169341 @default.
- W2105169341 hasPrimaryLocation W21051693411 @default.
- W2105169341 hasRelatedWork W1606027898 @default.
- W2105169341 hasRelatedWork W1964406565 @default.
- W2105169341 hasRelatedWork W2086052606 @default.
- W2105169341 hasRelatedWork W2095757660 @default.
- W2105169341 hasRelatedWork W2126866376 @default.
- W2105169341 hasRelatedWork W2140677556 @default.
- W2105169341 hasRelatedWork W2273013737 @default.
- W2105169341 hasRelatedWork W2359386786 @default.
- W2105169341 hasRelatedWork W2379720926 @default.
- W2105169341 hasRelatedWork W4221052601 @default.
- W2105169341 hasVolume "27" @default.
- W2105169341 isParatext "false" @default.
- W2105169341 isRetracted "false" @default.
- W2105169341 magId "2105169341" @default.
- W2105169341 workType "article" @default.