Matches in SemOpenAlex for { <https://semopenalex.org/work/W2133406688> ?p ?o ?g. }
- W2133406688 endingPage "1514" @default.
- W2133406688 startingPage "1497" @default.
- W2133406688 abstract "Sensitive high-resolution ion microprobe (SHRIMP) analyses of zircon from granites of the medium-high grade Aspromonte–Peloritani Unit, Calabria–Peloritani Orogen (CPO), southern Italy, show that one of the minor trondhjemites (313·7 ± 3·5 Ma) represents the earliest identified occurrence of Late Hercynian peraluminous igneous rocks in the CPO, predating the emplacement of the more common peraluminous leucogranodiorites by about 14 Myr. Some of the trondhjemite zircon grains contain small cores with ages of about 2·45 Ga, 625 Ma and 490 Ma, consistent with the presence of a sediment component in the magma. A newly dated leucogranodiorite (300·2 ± 3·8 Ma) is rich in inherited zircon. Cores with ages of about 2·36 Ga, 870 Ma, 630 Ma, 545 Ma and 460 Ma are overgrown by two generations of Hercynian igneous zircon, the first with moderate to high Th/U (up to 1· 67), and the second with low Th/U (< 0·1). The overgrowths probably crystallized from magmas of two compositions, the first metaluminous and the second peraluminous. This could indicate either magma mixing or, more probably, crystallization in a single, evolving magma. In either case, the leucogranodiorite magma is considered to have been the product of anatexis of a metasedimentary source. Differences in the inherited zircon age spectra, and the relatively small amount of inheritance in the trondhjemite, indicate that the trondhjemite and leucogranodiorite are unlikely to be genetically related. The ages of the inherited zircons are consistent with the sedimentary component in both magmas being derived from North Africa, with a possible contribution from Pan-African granitoids similar to those exposed in southern Calabria." @default.
- W2133406688 created "2016-06-24" @default.
- W2133406688 creator A5032650106 @default.
- W2133406688 creator A5047340697 @default.
- W2133406688 creator A5079465982 @default.
- W2133406688 creator A5085825108 @default.
- W2133406688 date "2008-07-07" @default.
- W2133406688 modified "2023-10-16" @default.
- W2133406688 title "Crustal Contributions to Late Hercynian Peraluminous Magmatism in the Southern Calabria-Peloritani Orogen, Southern Italy: Petrogenetic Inferences and the Gondwana Connection" @default.
- W2133406688 cites W1967004471 @default.
- W2133406688 cites W1967105963 @default.
- W2133406688 cites W1967572363 @default.
- W2133406688 cites W1977391626 @default.
- W2133406688 cites W1981028951 @default.
- W2133406688 cites W1991202690 @default.
- W2133406688 cites W1993236627 @default.
- W2133406688 cites W1994445295 @default.
- W2133406688 cites W1996507704 @default.
- W2133406688 cites W1999310213 @default.
- W2133406688 cites W2001135552 @default.
- W2133406688 cites W2003361831 @default.
- W2133406688 cites W2006584961 @default.
- W2133406688 cites W2014941046 @default.
- W2133406688 cites W2033966736 @default.
- W2133406688 cites W2043479761 @default.
- W2133406688 cites W2046961523 @default.
- W2133406688 cites W2054090861 @default.
- W2133406688 cites W2062703863 @default.
- W2133406688 cites W2072229475 @default.
- W2133406688 cites W2075751020 @default.
- W2133406688 cites W2085750254 @default.
- W2133406688 cites W2088519109 @default.
- W2133406688 cites W2088727955 @default.
- W2133406688 cites W2091795750 @default.
- W2133406688 cites W2095878716 @default.
- W2133406688 cites W2096684737 @default.
- W2133406688 cites W2098450639 @default.
- W2133406688 cites W2099819294 @default.
- W2133406688 cites W2102422895 @default.
- W2133406688 cites W2110400281 @default.
- W2133406688 cites W2114276383 @default.
- W2133406688 cites W2114440458 @default.
- W2133406688 cites W2125585433 @default.
- W2133406688 cites W2129531693 @default.
- W2133406688 cites W2139326036 @default.
- W2133406688 cites W2145604970 @default.
- W2133406688 cites W2147888749 @default.
- W2133406688 cites W2148448581 @default.
- W2133406688 cites W2151768794 @default.
- W2133406688 cites W2152848429 @default.
- W2133406688 cites W2162607179 @default.
- W2133406688 cites W2165805480 @default.
- W2133406688 cites W2317096966 @default.
- W2133406688 cites W2486708655 @default.
- W2133406688 cites W2588959757 @default.
- W2133406688 cites W2605589018 @default.
- W2133406688 cites W4246449801 @default.
- W2133406688 cites W4247876020 @default.
- W2133406688 doi "https://doi.org/10.1093/petrology/egn035" @default.
- W2133406688 hasPublicationYear "2008" @default.
- W2133406688 type Work @default.
- W2133406688 sameAs 2133406688 @default.
- W2133406688 citedByCount "47" @default.
- W2133406688 countsByYear W21334066882012 @default.
- W2133406688 countsByYear W21334066882013 @default.
- W2133406688 countsByYear W21334066882014 @default.
- W2133406688 countsByYear W21334066882015 @default.
- W2133406688 countsByYear W21334066882016 @default.
- W2133406688 countsByYear W21334066882017 @default.
- W2133406688 countsByYear W21334066882018 @default.
- W2133406688 countsByYear W21334066882019 @default.
- W2133406688 countsByYear W21334066882020 @default.
- W2133406688 countsByYear W21334066882021 @default.
- W2133406688 countsByYear W21334066882022 @default.
- W2133406688 countsByYear W21334066882023 @default.
- W2133406688 crossrefType "journal-article" @default.
- W2133406688 hasAuthorship W2133406688A5032650106 @default.
- W2133406688 hasAuthorship W2133406688A5047340697 @default.
- W2133406688 hasAuthorship W2133406688A5079465982 @default.
- W2133406688 hasAuthorship W2133406688A5085825108 @default.
- W2133406688 hasBestOaLocation W21334066882 @default.
- W2133406688 hasConcept C120806208 @default.
- W2133406688 hasConcept C127313418 @default.
- W2133406688 hasConcept C151730666 @default.
- W2133406688 hasConcept C162973429 @default.
- W2133406688 hasConcept C167236342 @default.
- W2133406688 hasConcept C17409809 @default.
- W2133406688 hasConcept C183222429 @default.
- W2133406688 hasConcept C2776698055 @default.
- W2133406688 hasConcept C2778849375 @default.
- W2133406688 hasConcept C2779604315 @default.
- W2133406688 hasConcept C2781148125 @default.
- W2133406688 hasConcept C42787717 @default.
- W2133406688 hasConcept C5900021 @default.
- W2133406688 hasConcept C77928131 @default.
- W2133406688 hasConcept C79572550 @default.
- W2133406688 hasConceptScore W2133406688C120806208 @default.
- W2133406688 hasConceptScore W2133406688C127313418 @default.