FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2079463364> ?p ?o ?g. }

• W2079463364 endingPage "495" @default.
• W2079463364 startingPage "495" @default.
• W2079463364 abstract "Research Article| June 01, 2008 Cause and evolution of intraplate orogeny in Australia S. Dyksterhuis; S. Dyksterhuis 1EarthByte Group, School of Geosciences, Building H11, The University of Sydney, New South Wales 2006, Australia Search for other works by this author on: GSW Google Scholar R.D. Müller R.D. Müller * 1EarthByte Group, School of Geosciences, Building H11, The University of Sydney, New South Wales 2006, Australia *E-mail: d.muller@usyd.edu.au. Search for other works by this author on: GSW Google Scholar Geology (2008) 36 (6): 495–498. https://doi.org/10.1130/G24536A.1 Article history received: 22 Nov 2007 rev-recd: 18 Feb 2008 accepted: 25 Feb 2008 first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation S. Dyksterhuis, R.D. Müller; Cause and evolution of intraplate orogeny in Australia. Geology 2008;; 36 (6): 495–498. doi: https://doi.org/10.1130/G24536A.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 Intraplate orogeny remains an enigmatic process in terms of plate tectonics. Regional continental stress fields agree well with stress orientations predicted by the main forces driving and resisting plate motion. However, regional continental stress fields fail to explain major localized compressive plate deformation in continental interiors far away from plate boundaries. Global or plate-wide intraplate stress models typically assume a laterally homogeneous plate rheology and are confined to modeling the present, without addressing the antiquity of the current stress field. An understanding of intraplate stress and deformation requires the linking of spatial variations in continental rheology with time-dependent plate geometry and driving forces. Here we demonstrate how the complex interplay between juxtaposed weak and strong geological provinces and changes in far-field plate boundary forces has caused intra-plate orogenesis and tectonic reactivation in southeastern Australia during the Tertiary. Our findings are contrary to the opinion that continental interiors are insensitive to compression at plate margins, and help to explain the mechanisms causing intraplate orogenesis. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
• W2079463364 created "2016-06-24" @default.
• W2079463364 creator A5020479987 @default.
• W2079463364 creator A5042746575 @default.
• W2079463364 date "2008-01-01" @default.
• W2079463364 modified "2023-10-08" @default.
• W2079463364 title "Cause and evolution of intraplate orogeny in Australia" @default.
• W2079463364 cites W1565077474 @default.
• W2079463364 cites W167869813 @default.
• W2079463364 cites W1859934969 @default.
• W2079463364 cites W1891985660 @default.
• W2079463364 cites W1964990445 @default.
• W2079463364 cites W1976467450 @default.
• W2079463364 cites W1984547753 @default.
• W2079463364 cites W1998801453 @default.
• W2079463364 cites W2004293503 @default.
• W2079463364 cites W2006280751 @default.
• W2079463364 cites W2009922398 @default.
• W2079463364 cites W2021597572 @default.
• W2079463364 cites W2062439770 @default.
• W2079463364 cites W2070669093 @default.
• W2079463364 cites W2077743957 @default.
• W2079463364 cites W2092948140 @default.
• W2079463364 cites W2095048151 @default.
• W2079463364 cites W2098965205 @default.
• W2079463364 cites W2104364549 @default.
• W2079463364 cites W2108952814 @default.
• W2079463364 cites W2119605296 @default.
• W2079463364 cites W2123844571 @default.
• W2079463364 cites W2130836619 @default.
• W2079463364 cites W2135122208 @default.
• W2079463364 cites W2143046705 @default.
• W2079463364 cites W2158427587 @default.
• W2079463364 cites W2162265875 @default.
• W2079463364 cites W2291873642 @default.
• W2079463364 cites W2336091768 @default.
• W2079463364 cites W2392835767 @default.
• W2079463364 cites W2749900705 @default.
• W2079463364 doi "https://doi.org/10.1130/g24536a.1" @default.
• W2079463364 hasPublicationYear "2008" @default.
• W2079463364 type Work @default.
• W2079463364 sameAs 2079463364 @default.
• W2079463364 citedByCount "72" @default.
• W2079463364 countsByYear W20794633642012 @default.
• W2079463364 countsByYear W20794633642013 @default.
• W2079463364 countsByYear W20794633642014 @default.
• W2079463364 countsByYear W20794633642015 @default.
• W2079463364 countsByYear W20794633642016 @default.
• W2079463364 countsByYear W20794633642017 @default.
• W2079463364 countsByYear W20794633642018 @default.
• W2079463364 countsByYear W20794633642019 @default.
• W2079463364 countsByYear W20794633642020 @default.
• W2079463364 countsByYear W20794633642021 @default.
• W2079463364 countsByYear W20794633642023 @default.
• W2079463364 crossrefType "journal-article" @default.
• W2079463364 hasAuthorship W2079463364A5020479987 @default.
• W2079463364 hasAuthorship W2079463364A5042746575 @default.
• W2079463364 hasConcept C119477230 @default.
• W2079463364 hasConcept C127313418 @default.
• W2079463364 hasConcept C151730666 @default.
• W2079463364 hasConcept C161191863 @default.
• W2079463364 hasConcept C199360897 @default.
• W2079463364 hasConcept C2777241186 @default.
• W2079463364 hasConcept C2778447006 @default.
• W2079463364 hasConcept C2778805511 @default.
• W2079463364 hasConcept C41008148 @default.
• W2079463364 hasConcept C77928131 @default.
• W2079463364 hasConcept C84786313 @default.
• W2079463364 hasConceptScore W2079463364C119477230 @default.
• W2079463364 hasConceptScore W2079463364C127313418 @default.
• W2079463364 hasConceptScore W2079463364C151730666 @default.
• W2079463364 hasConceptScore W2079463364C161191863 @default.
• W2079463364 hasConceptScore W2079463364C199360897 @default.
• W2079463364 hasConceptScore W2079463364C2777241186 @default.
• W2079463364 hasConceptScore W2079463364C2778447006 @default.
• W2079463364 hasConceptScore W2079463364C2778805511 @default.
• W2079463364 hasConceptScore W2079463364C41008148 @default.
• W2079463364 hasConceptScore W2079463364C77928131 @default.
• W2079463364 hasConceptScore W2079463364C84786313 @default.
• W2079463364 hasIssue "6" @default.
• W2079463364 hasLocation W20794633641 @default.
• W2079463364 hasOpenAccess W2079463364 @default.
• W2079463364 hasPrimaryLocation W20794633641 @default.
• W2079463364 hasRelatedWork W2038288419 @default.
• W2079463364 hasRelatedWork W2243147761 @default.
• W2079463364 hasRelatedWork W2348255584 @default.
• W2079463364 hasRelatedWork W2355393803 @default.
• W2079463364 hasRelatedWork W2356674837 @default.
• W2079463364 hasRelatedWork W2390589831 @default.
• W2079463364 hasRelatedWork W2392730771 @default.
• W2079463364 hasRelatedWork W2991519324 @default.
• W2079463364 hasRelatedWork W3037196366 @default.
• W2079463364 hasRelatedWork W42837437 @default.
• W2079463364 hasVolume "36" @default.
• W2079463364 isParatext "false" @default.
• W2079463364 isRetracted "false" @default.
• W2079463364 magId "2079463364" @default.
• W2079463364 workType "article" @default.