Matches in SemOpenAlex for { <https://semopenalex.org/work/W2074857191> ?p ?o ?g. }
- W2074857191 endingPage "1146" @default.
- W2074857191 startingPage "1143" @default.
- W2074857191 abstract "Research Article| December 01, 2011 Metamorphic replacement of mineral inclusions in detrital zircon from Jack Hills, Australia: Implications for the Hadean Earth Birger Rasmussen; Birger Rasmussen 1Department of Applied Geology, Curtin University, Kent Street, Bentley, WA 6102, Australia Search for other works by this author on: GSW Google Scholar Ian R. Fletcher; Ian R. Fletcher 1Department of Applied Geology, Curtin University, Kent Street, Bentley, WA 6102, Australia Search for other works by this author on: GSW Google Scholar Janet R. Muhling; Janet R. Muhling 2Centre for Microscopy, Characterisation and Analysis, University of Western Australia, 35 Stirling Highway, Crawley, WA 6009, Australia Search for other works by this author on: GSW Google Scholar Courtney J. Gregory; Courtney J. Gregory 1Department of Applied Geology, Curtin University, Kent Street, Bentley, WA 6102, Australia Search for other works by this author on: GSW Google Scholar Simon A. Wilde Simon A. Wilde 1Department of Applied Geology, Curtin University, Kent Street, Bentley, WA 6102, Australia Search for other works by this author on: GSW Google Scholar Geology (2011) 39 (12): 1143–1146. https://doi.org/10.1130/G32554.1 Article history received: 14 Jun 2011 rev-recd: 05 Jul 2011 accepted: 11 Jul 2011 first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share MailTo Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation Birger Rasmussen, Ian R. Fletcher, Janet R. Muhling, Courtney J. Gregory, Simon A. Wilde; Metamorphic replacement of mineral inclusions in detrital zircon from Jack Hills, Australia: Implications for the Hadean Earth. Geology 2011;; 39 (12): 1143–1146. doi: https://doi.org/10.1130/G32554.1 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 The Hadean (before 4.0 Ga) crust has long been considered to comprise mainly primitive mafic and ultramafic rocks. However, mineral inclusions in detrital zircons as old as 4.4 Ga from Jack Hills, Australia, have been interpreted to be magmatic and to provide evidence for extensive granitic crust. In situ U-Pb dating of monazite and xenotime inclusions in 4.25–3.35 Ga detrital zircons from Jack Hills shows that these inclusions are not magmatic, but formed during metamorphism at either 2.68 Ga or 0.8 Ga. Monazite-xenotime thermometry of intergrowths in the inclusions and the quartz-muscovite rock matrix constrain temperatures to between 420–475 °C, corresponding with conditions during peak regional metamorphism. Petrography and U-Pb geochronology of zircon inclusions from other localities show that the replacement of primary inclusions may commence in the igneous host rock and continue through weathering, sedimentation, and diagenesis. With increasing metamorphic grade, the inclusion assemblage increasingly reflects the composition of the rock matrix. In Jack Hills, most of the inclusions have the same composition and abundances as the metamorphic matrix, consistent with their formation during metamorphism. The titanium content of quartz inclusions indicates formation temperatures of 350–490 °C, supporting a metamorphic origin. Several lines of evidence indicate that at least some of the muscovite inclusions are also secondary. The lack of apatite inclusions in zircons from Jack Hills, relative to zircon in common granitic rocks, suggests that secondary minerals may have replaced primary apatite. Thus, detrital zircon may not be impermeable to post-depositional fluids, raising doubts about the use of the mineral inclusions they contain to infer initial magma chemistry. These results call for a reassessment of the source melts of the Hadean zircons and the composition of the earliest crust. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
- W2074857191 created "2016-06-24" @default.
- W2074857191 creator A5004680297 @default.
- W2074857191 creator A5013650435 @default.
- W2074857191 creator A5026256786 @default.
- W2074857191 creator A5055907746 @default.
- W2074857191 creator A5063587791 @default.
- W2074857191 date "2011-12-01" @default.
- W2074857191 modified "2023-09-23" @default.
- W2074857191 title "Metamorphic replacement of mineral inclusions in detrital zircon from Jack Hills, Australia: Implications for the Hadean Earth" @default.
- W2074857191 cites W1615737483 @default.
- W2074857191 cites W1973986300 @default.
- W2074857191 cites W1981788146 @default.
- W2074857191 cites W1988503846 @default.
- W2074857191 cites W1997233054 @default.
- W2074857191 cites W1998886247 @default.
- W2074857191 cites W2002216612 @default.
- W2074857191 cites W2006234070 @default.
- W2074857191 cites W2013451364 @default.
- W2074857191 cites W2021343197 @default.
- W2074857191 cites W2026000927 @default.
- W2074857191 cites W2052636445 @default.
- W2074857191 cites W2059277213 @default.
- W2074857191 cites W2069294002 @default.
- W2074857191 cites W2071654977 @default.
- W2074857191 cites W2074530210 @default.
- W2074857191 cites W2079101766 @default.
- W2074857191 cites W2087605997 @default.
- W2074857191 cites W2136852838 @default.
- W2074857191 cites W2140930922 @default.
- W2074857191 cites W2342547907 @default.
- W2074857191 doi "https://doi.org/10.1130/g32554.1" @default.
- W2074857191 hasPublicationYear "2011" @default.
- W2074857191 type Work @default.
- W2074857191 sameAs 2074857191 @default.
- W2074857191 citedByCount "92" @default.
- W2074857191 countsByYear W20748571912012 @default.
- W2074857191 countsByYear W20748571912013 @default.
- W2074857191 countsByYear W20748571912014 @default.
- W2074857191 countsByYear W20748571912015 @default.
- W2074857191 countsByYear W20748571912016 @default.
- W2074857191 countsByYear W20748571912017 @default.
- W2074857191 countsByYear W20748571912018 @default.
- W2074857191 countsByYear W20748571912019 @default.
- W2074857191 countsByYear W20748571912020 @default.
- W2074857191 countsByYear W20748571912021 @default.
- W2074857191 countsByYear W20748571912022 @default.
- W2074857191 countsByYear W20748571912023 @default.
- W2074857191 crossrefType "journal-article" @default.
- W2074857191 hasAuthorship W2074857191A5004680297 @default.
- W2074857191 hasAuthorship W2074857191A5013650435 @default.
- W2074857191 hasAuthorship W2074857191A5026256786 @default.
- W2074857191 hasAuthorship W2074857191A5055907746 @default.
- W2074857191 hasAuthorship W2074857191A5063587791 @default.
- W2074857191 hasConcept C112764850 @default.
- W2074857191 hasConcept C127313418 @default.
- W2074857191 hasConcept C150999391 @default.
- W2074857191 hasConcept C151730666 @default.
- W2074857191 hasConcept C161191863 @default.
- W2074857191 hasConcept C166957645 @default.
- W2074857191 hasConcept C199360897 @default.
- W2074857191 hasConcept C26687426 @default.
- W2074857191 hasConcept C2777898519 @default.
- W2074857191 hasConcept C2778447006 @default.
- W2074857191 hasConcept C2778805511 @default.
- W2074857191 hasConcept C2778849375 @default.
- W2074857191 hasConcept C2779483780 @default.
- W2074857191 hasConcept C37523158 @default.
- W2074857191 hasConcept C41008148 @default.
- W2074857191 hasConcept C52119013 @default.
- W2074857191 hasConcept C77928131 @default.
- W2074857191 hasConcept C95457728 @default.
- W2074857191 hasConceptScore W2074857191C112764850 @default.
- W2074857191 hasConceptScore W2074857191C127313418 @default.
- W2074857191 hasConceptScore W2074857191C150999391 @default.
- W2074857191 hasConceptScore W2074857191C151730666 @default.
- W2074857191 hasConceptScore W2074857191C161191863 @default.
- W2074857191 hasConceptScore W2074857191C166957645 @default.
- W2074857191 hasConceptScore W2074857191C199360897 @default.
- W2074857191 hasConceptScore W2074857191C26687426 @default.
- W2074857191 hasConceptScore W2074857191C2777898519 @default.
- W2074857191 hasConceptScore W2074857191C2778447006 @default.
- W2074857191 hasConceptScore W2074857191C2778805511 @default.
- W2074857191 hasConceptScore W2074857191C2778849375 @default.
- W2074857191 hasConceptScore W2074857191C2779483780 @default.
- W2074857191 hasConceptScore W2074857191C37523158 @default.
- W2074857191 hasConceptScore W2074857191C41008148 @default.
- W2074857191 hasConceptScore W2074857191C52119013 @default.
- W2074857191 hasConceptScore W2074857191C77928131 @default.
- W2074857191 hasConceptScore W2074857191C95457728 @default.
- W2074857191 hasIssue "12" @default.
- W2074857191 hasLocation W20748571911 @default.
- W2074857191 hasOpenAccess W2074857191 @default.
- W2074857191 hasPrimaryLocation W20748571911 @default.
- W2074857191 hasRelatedWork W1968565099 @default.
- W2074857191 hasRelatedWork W1986088847 @default.
- W2074857191 hasRelatedWork W2061582730 @default.
- W2074857191 hasRelatedWork W2063408010 @default.