FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2020116870> ?p ?o ?g. }

• W2020116870 endingPage "1082" @default.
• W2020116870 startingPage "1079" @default.
• W2020116870 abstract "Research Article| December 01, 2012 Phanerozoic sanukitoids from Caledonian Scotland: Implications for Archean subduction Mike Fowler; Mike Fowler * 1Earth and Environmental Sciences, University of Portsmouth, Burnaby Building, Burnaby Road, Portsmouth PO1 3QL, UK *E-mail: mike.fowler@port.ac.uk. Search for other works by this author on: GSW Google Scholar Hugh Rollinson Hugh Rollinson 2School of Science, University of Derby, Kedleston Road, Derby DE22 1GB, UK Search for other works by this author on: GSW Google Scholar Author and Article Information Mike Fowler * 1Earth and Environmental Sciences, University of Portsmouth, Burnaby Building, Burnaby Road, Portsmouth PO1 3QL, UK Hugh Rollinson 2School of Science, University of Derby, Kedleston Road, Derby DE22 1GB, UK *E-mail: mike.fowler@port.ac.uk. Publisher: Geological Society of America Received: 03 Mar 2012 Revision Received: 14 May 2012 Accepted: 16 May 2012 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2012 Geological Society of America Geology (2012) 40 (12): 1079–1082. https://doi.org/10.1130/G33371.1 Article history Received: 03 Mar 2012 Revision Received: 14 May 2012 Accepted: 16 May 2012 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Mike Fowler, Hugh Rollinson; Phanerozoic sanukitoids from Caledonian Scotland: Implications for Archean subduction. Geology 2012;; 40 (12): 1079–1082. doi: https://doi.org/10.1130/G33371.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Sanukitoids represent a volumetrically minor but important series of Neoarchean granitoids enriched in large-ion lithophile elements (e.g., Ba, Sr, and light rare earth elements), and with relatively high compatible elements (e.g., Mg, Ni, and Cr). Petrogenetic models have favored an origin in the suprasubduction mantle wedge, so their sudden appearance ca. 2.95–2.68 Ga has made them central to the ongoing debate about the beginnings of modern plate tectonics. Caledonian high Ba-Sr granites from the Northern Highlands of Scotland are petrological and compositional equivalents. The Caledonian examples have not undergone subsequent reworking, and their petrogenetic setting can be used to inform genetic models for sanukitoids. Prolonged subduction preceded emplacement of the high Ba-Sr granites in a short interval (∼10 Ma) at the end of the Caledonian orogeny. Sediment subduction was responsible for elemental and isotopic enrichments and slab breakoff triggered melting in the subcontinental lithospheric mantle. This implies that during the Neoarchean the evolving tectonothermal regime moved the locus of melting from the basaltic slab to the sediment-infused mantle wedge, creating the first subcontinental lithospheric mantle. Sanukitoids may then have resulted from widespread, closely subsequent slab-breakoff events, producing evolved magmas by familiar fractionation mechanisms. Careful study of secular variations in high Ba-Sr magmas could constrain the evolution of the subcontinental lithosphere. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
• W2020116870 created "2016-06-24" @default.
• W2020116870 creator A5038411305 @default.
• W2020116870 creator A5083269164 @default.
• W2020116870 date "2012-12-01" @default.
• W2020116870 modified "2023-10-16" @default.
• W2020116870 title "Phanerozoic sanukitoids from Caledonian Scotland: Implications for Archean subduction" @default.
• W2020116870 cites W1964047299 @default.
• W2020116870 cites W1967082613 @default.
• W2020116870 cites W1974416183 @default.
• W2020116870 cites W1975546571 @default.
• W2020116870 cites W1977638370 @default.
• W2020116870 cites W1982589593 @default.
• W2020116870 cites W2003032844 @default.
• W2020116870 cites W2009615347 @default.
• W2020116870 cites W2011065740 @default.
• W2020116870 cites W2014384293 @default.
• W2020116870 cites W2020324113 @default.
• W2020116870 cites W2031323213 @default.
• W2020116870 cites W2031844927 @default.
• W2020116870 cites W2052095461 @default.
• W2020116870 cites W2056501220 @default.
• W2020116870 cites W2060447317 @default.
• W2020116870 cites W2069762342 @default.
• W2020116870 cites W2070727611 @default.
• W2020116870 cites W2073607775 @default.
• W2020116870 cites W2077704118 @default.
• W2020116870 cites W2080843712 @default.
• W2020116870 cites W2092151651 @default.
• W2020116870 cites W2092235841 @default.
• W2020116870 cites W2102199274 @default.
• W2020116870 cites W2108971421 @default.
• W2020116870 cites W2127940040 @default.
• W2020116870 cites W2132669405 @default.
• W2020116870 cites W2140134802 @default.
• W2020116870 cites W2169394717 @default.
• W2020116870 cites W2332879341 @default.
• W2020116870 doi "https://doi.org/10.1130/g33371.1" @default.
• W2020116870 hasPublicationYear "2012" @default.
• W2020116870 type Work @default.
• W2020116870 sameAs 2020116870 @default.
• W2020116870 citedByCount "67" @default.
• W2020116870 countsByYear W20201168702014 @default.
• W2020116870 countsByYear W20201168702015 @default.
• W2020116870 countsByYear W20201168702016 @default.
• W2020116870 countsByYear W20201168702017 @default.
• W2020116870 countsByYear W20201168702018 @default.
• W2020116870 countsByYear W20201168702019 @default.
• W2020116870 countsByYear W20201168702020 @default.
• W2020116870 countsByYear W20201168702021 @default.
• W2020116870 countsByYear W20201168702022 @default.
• W2020116870 countsByYear W20201168702023 @default.
• W2020116870 crossrefType "journal-article" @default.
• W2020116870 hasAuthorship W2020116870A5038411305 @default.
• W2020116870 hasAuthorship W2020116870A5083269164 @default.
• W2020116870 hasConcept C109007969 @default.
• W2020116870 hasConcept C127313418 @default.
• W2020116870 hasConcept C149347711 @default.
• W2020116870 hasConcept C151730666 @default.
• W2020116870 hasConcept C161191863 @default.
• W2020116870 hasConcept C166957645 @default.
• W2020116870 hasConcept C167570900 @default.
• W2020116870 hasConcept C2778805511 @default.
• W2020116870 hasConcept C41008148 @default.
• W2020116870 hasConcept C58097730 @default.
• W2020116870 hasConcept C73707237 @default.
• W2020116870 hasConcept C77928131 @default.
• W2020116870 hasConcept C95457728 @default.
• W2020116870 hasConceptScore W2020116870C109007969 @default.
• W2020116870 hasConceptScore W2020116870C127313418 @default.
• W2020116870 hasConceptScore W2020116870C149347711 @default.
• W2020116870 hasConceptScore W2020116870C151730666 @default.
• W2020116870 hasConceptScore W2020116870C161191863 @default.
• W2020116870 hasConceptScore W2020116870C166957645 @default.
• W2020116870 hasConceptScore W2020116870C167570900 @default.
• W2020116870 hasConceptScore W2020116870C2778805511 @default.
• W2020116870 hasConceptScore W2020116870C41008148 @default.
• W2020116870 hasConceptScore W2020116870C58097730 @default.
• W2020116870 hasConceptScore W2020116870C73707237 @default.
• W2020116870 hasConceptScore W2020116870C77928131 @default.
• W2020116870 hasConceptScore W2020116870C95457728 @default.
• W2020116870 hasIssue "12" @default.
• W2020116870 hasLocation W20201168701 @default.
• W2020116870 hasOpenAccess W2020116870 @default.
• W2020116870 hasPrimaryLocation W20201168701 @default.
• W2020116870 hasRelatedWork W12735650 @default.
• W2020116870 hasRelatedWork W1970042240 @default.
• W2020116870 hasRelatedWork W2015603624 @default.
• W2020116870 hasRelatedWork W2030302093 @default.
• W2020116870 hasRelatedWork W2106751816 @default.
• W2020116870 hasRelatedWork W2107520839 @default.
• W2020116870 hasRelatedWork W2119695127 @default.
• W2020116870 hasRelatedWork W2914659861 @default.
• W2020116870 hasRelatedWork W3143933168 @default.
• W2020116870 hasRelatedWork W4237866904 @default.
• W2020116870 hasVolume "40" @default.
• W2020116870 isParatext "false" @default.
• W2020116870 isRetracted "false" @default.

• next