FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2023176422> ?p ?o ?g. }

• W2023176422 endingPage "490" @default.
• W2023176422 startingPage "475" @default.
• W2023176422 abstract "Abstract The East African Orogen formed as a result of collision between portions of East and West Gondwanaland as the Mozambique Ocean closed in Late Neoproterozoic time, but it is not known exactly when. We use distinctive chemical and isotopic composition of deformed ‘schistose’ dykes in southern Israel to argue that this collision occurred after about 630 Ma, when the dykes were emplaced. These magmas had compositions of basaltic andesites and andesites but had high Mg# (100 Mg/Mg+Fe; 55–70 ppm), Ni (70–240 ppm), and Cr (100–400 ppm) indicating that the most primitive samples were in equilibrium with mantle peridotite; evolved samples suffered modest fractionation. The schistose dykes are a medium-K, calc-alkaline suite, strongly enriched in light rare earth elements and depleted in heavy rare earth elements. They are high-magnesium andesites and are similar to low-Ca type 2 boninites; similar magmas today only form over active subduction zones. The schistose dykes have non-radiogenic initial 87Sr/86Sr (0.7026–0.7033) and radiogenic 143Nd/144Nd, with ϵNd(630 Ma) of +2.7 to +4.9 and TDM=0.77–0.94 Ga. Hf isotopic compositions (ϵHf(630 Ma)=+6.8 to +8.8) confirm the juvenile nature of these magmas. The dykes are closely related to a nearby quartz diorite, although it is not clear whether the dykes represent magma that fed into a magma body now filled with the quartz diorite, or issued from it. The generation of high-Mg andesite magma at 630 Ma involved reactive porous flow of a slab-derived melt through the mantle, requiring an active subduction zone, and strongly suggesting that young, hot seafloor – perhaps the spreading ridge of the Mozambique Ocean – was subducted. This indicates that collision between components of E. and W. Gondwana to form the East African Orogen must have occurred more recently than 630 Ma." @default.
• W2023176422 created "2016-06-24" @default.
• W2023176422 creator A5026781865 @default.
• W2023176422 creator A5030306759 @default.
• W2023176422 creator A5035240990 @default.
• W2023176422 creator A5036502893 @default.
• W2023176422 creator A5046237493 @default.
• W2023176422 creator A5060024339 @default.
• W2023176422 creator A5078264726 @default.
• W2023176422 date "2004-02-01" @default.
• W2023176422 modified "2023-09-26" @default.
• W2023176422 title "A Late Neoproterozoic (∼630 Ma) high-magnesium andesite suite from southern Israel: implications for the consolidation of Gondwanaland" @default.
• W2023176422 cites W1967082613 @default.
• W2023176422 cites W1973800976 @default.
• W2023176422 cites W1975864669 @default.
• W2023176422 cites W1977705982 @default.
• W2023176422 cites W1983596468 @default.
• W2023176422 cites W1985153077 @default.
• W2023176422 cites W1993449388 @default.
• W2023176422 cites W2000789282 @default.
• W2023176422 cites W2001393837 @default.
• W2023176422 cites W2002356846 @default.
• W2023176422 cites W2009058679 @default.
• W2023176422 cites W2017299757 @default.
• W2023176422 cites W2020304604 @default.
• W2023176422 cites W2020317492 @default.
• W2023176422 cites W2026590347 @default.
• W2023176422 cites W2026722663 @default.
• W2023176422 cites W2031673333 @default.
• W2023176422 cites W2043694977 @default.
• W2023176422 cites W2044609027 @default.
• W2023176422 cites W2046593869 @default.
• W2023176422 cites W2058741861 @default.
• W2023176422 cites W2059506020 @default.
• W2023176422 cites W2068299560 @default.
• W2023176422 cites W2072833969 @default.
• W2023176422 cites W2075199408 @default.
• W2023176422 cites W2077291658 @default.
• W2023176422 cites W2079765078 @default.
• W2023176422 cites W2081673195 @default.
• W2023176422 cites W2083239370 @default.
• W2023176422 cites W2103240374 @default.
• W2023176422 cites W2103579604 @default.
• W2023176422 cites W2107282719 @default.
• W2023176422 cites W2119438235 @default.
• W2023176422 cites W2120852101 @default.
• W2023176422 cites W2127039475 @default.
• W2023176422 cites W2142266349 @default.
• W2023176422 cites W2150049829 @default.
• W2023176422 cites W2151676289 @default.
• W2023176422 cites W2154965338 @default.
• W2023176422 cites W2157099954 @default.
• W2023176422 cites W2164957174 @default.
• W2023176422 cites W2170319829 @default.
• W2023176422 cites W2174216460 @default.
• W2023176422 cites W2325019720 @default.
• W2023176422 cites W3207805732 @default.
• W2023176422 cites W4205749704 @default.
• W2023176422 doi "https://doi.org/10.1016/s0012-821x(03)00635-6" @default.
• W2023176422 hasPublicationYear "2004" @default.
• W2023176422 type Work @default.
• W2023176422 sameAs 2023176422 @default.
• W2023176422 citedByCount "67" @default.
• W2023176422 countsByYear W20231764222012 @default.
• W2023176422 countsByYear W20231764222013 @default.
• W2023176422 countsByYear W20231764222014 @default.
• W2023176422 countsByYear W20231764222015 @default.
• W2023176422 countsByYear W20231764222016 @default.
• W2023176422 countsByYear W20231764222017 @default.
• W2023176422 countsByYear W20231764222018 @default.
• W2023176422 countsByYear W20231764222019 @default.
• W2023176422 countsByYear W20231764222020 @default.
• W2023176422 countsByYear W20231764222021 @default.
• W2023176422 countsByYear W20231764222022 @default.
• W2023176422 crossrefType "journal-article" @default.
• W2023176422 hasAuthorship W2023176422A5026781865 @default.
• W2023176422 hasAuthorship W2023176422A5030306759 @default.
• W2023176422 hasAuthorship W2023176422A5035240990 @default.
• W2023176422 hasAuthorship W2023176422A5036502893 @default.
• W2023176422 hasAuthorship W2023176422A5046237493 @default.
• W2023176422 hasAuthorship W2023176422A5060024339 @default.
• W2023176422 hasAuthorship W2023176422A5078264726 @default.
• W2023176422 hasConcept C120806208 @default.
• W2023176422 hasConcept C121955636 @default.
• W2023176422 hasConcept C127313418 @default.
• W2023176422 hasConcept C144133560 @default.
• W2023176422 hasConcept C151730666 @default.
• W2023176422 hasConcept C166957645 @default.
• W2023176422 hasConcept C17409809 @default.
• W2023176422 hasConcept C192241223 @default.
• W2023176422 hasConcept C2776014549 @default.
• W2023176422 hasConcept C36986328 @default.
• W2023176422 hasConcept C5900021 @default.
• W2023176422 hasConcept C79581498 @default.
• W2023176422 hasConcept C95457728 @default.
• W2023176422 hasConceptScore W2023176422C120806208 @default.
• W2023176422 hasConceptScore W2023176422C121955636 @default.
• W2023176422 hasConceptScore W2023176422C127313418 @default.

• next