FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2315399125> ?p ?o ?g. }

• W2315399125 endingPage "102" @default.
• W2315399125 startingPage "99" @default.
• W2315399125 abstract "Research Article| February 01, 2012 Tectonic subsidence of the Lomonosov Ridge Alexander N. Minakov; Alexander N. Minakov * 1Department of Earth Science, University of Bergen, Allegaten 41, NO-5007, Bergen, Norway *E-mails: Alexander.Minakov@geo.uib.no; Yury.Podladchikov@unil.ch. Search for other works by this author on: GSW Google Scholar Yury Yu. Podladchikov Yury Yu. Podladchikov * 2Faculty of Geosciences and Environment, University of Lausanne, CH-1015, Lausanne, Switzerland *E-mails: Alexander.Minakov@geo.uib.no; Yury.Podladchikov@unil.ch. Search for other works by this author on: GSW Google Scholar Author and Article Information Alexander N. Minakov * 1Department of Earth Science, University of Bergen, Allegaten 41, NO-5007, Bergen, Norway Yury Yu. Podladchikov * 2Faculty of Geosciences and Environment, University of Lausanne, CH-1015, Lausanne, Switzerland *E-mails: Alexander.Minakov@geo.uib.no; Yury.Podladchikov@unil.ch. Publisher: Geological Society of America Received: 11 May 2011 Revision Received: 01 Sep 2011 Accepted: 02 Sep 2011 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2012 Geological Society of America Geology (2012) 40 (2): 99–102. https://doi.org/10.1130/G32445.1 Article history Received: 11 May 2011 Revision Received: 01 Sep 2011 Accepted: 02 Sep 2011 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Alexander N. Minakov, Yury Yu. Podladchikov; Tectonic subsidence of the Lomonosov Ridge. Geology 2012;; 40 (2): 99–102. doi: https://doi.org/10.1130/G32445.1 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 Cenozoic sedimentary record revealed by the Integrated Ocean Drilling Program's Arctic Coring Expedition (ACEX) to the Lomonosov Ridge microcontinent in 2004 is characterized by an unconformity attributed to the period 44–18 Ma. According to conventional thermal kinematic models, the microcontinent should have subsided to >1 km depth owing to rifting and subsequent separation from the Barents–Kara Sea margin at 56 Ma. We propose an alternative model incorporating a simple pressure-temperature (P-T) relation for mantle density. Using this model, we can explain the missing stratigraphic section by post-breakup uplift and erosion. The pattern of linear magnetic anomalies and the spreading geometry imply that the generation of oceanic crust in the central Eurasia Basin could have been restricted and confined by non-volcanic thinning of the mantle lithosphere at an early stage (ca. 56–40 Ma). In response to a rise in temperature, the mantle mineral composition may have changed through breakdown of spinel peridotite and formation of less dense plagioclase peridotite. The consequence of lithosphere heating and related mineral phase transitions would be post-breakup uplift followed by rapid subsidence to the deep-water environment observed on the Lomonosov Ridge today. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
• W2315399125 created "2016-06-24" @default.
• W2315399125 creator A5030976970 @default.
• W2315399125 creator A5069200685 @default.
• W2315399125 date "2011-12-08" @default.
• W2315399125 modified "2023-09-27" @default.
• W2315399125 title "Tectonic subsidence of the Lomonosov Ridge" @default.
• W2315399125 cites W1983074253 @default.
• W2315399125 cites W2009572653 @default.
• W2315399125 cites W2020286870 @default.
• W2315399125 cites W2021754290 @default.
• W2315399125 cites W2027735940 @default.
• W2315399125 cites W2031145316 @default.
• W2315399125 cites W2038645351 @default.
• W2315399125 cites W2046640225 @default.
• W2315399125 cites W2080743915 @default.
• W2315399125 cites W2086259978 @default.
• W2315399125 cites W2093318992 @default.
• W2315399125 cites W2104956692 @default.
• W2315399125 cites W2123445693 @default.
• W2315399125 cites W2123741232 @default.
• W2315399125 cites W2124173619 @default.
• W2315399125 cites W2127080669 @default.
• W2315399125 cites W2140693720 @default.
• W2315399125 cites W2141229633 @default.
• W2315399125 cites W2166273297 @default.
• W2315399125 cites W2170609637 @default.
• W2315399125 doi "https://doi.org/10.1130/g32445.1" @default.
• W2315399125 hasPublicationYear "2011" @default.
• W2315399125 type Work @default.
• W2315399125 sameAs 2315399125 @default.
• W2315399125 citedByCount "12" @default.
• W2315399125 countsByYear W23153991252013 @default.
• W2315399125 countsByYear W23153991252014 @default.
• W2315399125 countsByYear W23153991252015 @default.
• W2315399125 countsByYear W23153991252016 @default.
• W2315399125 countsByYear W23153991252018 @default.
• W2315399125 countsByYear W23153991252019 @default.
• W2315399125 countsByYear W23153991252020 @default.
• W2315399125 countsByYear W23153991252022 @default.
• W2315399125 crossrefType "journal-article" @default.
• W2315399125 hasAuthorship W2315399125A5030976970 @default.
• W2315399125 hasAuthorship W2315399125A5069200685 @default.
• W2315399125 hasConcept C127313418 @default.
• W2315399125 hasConcept C136764020 @default.
• W2315399125 hasConcept C151730666 @default.
• W2315399125 hasConcept C161191863 @default.
• W2315399125 hasConcept C2778805511 @default.
• W2315399125 hasConcept C2779483780 @default.
• W2315399125 hasConcept C2780154274 @default.
• W2315399125 hasConcept C32277403 @default.
• W2315399125 hasConcept C41008148 @default.
• W2315399125 hasConceptScore W2315399125C127313418 @default.
• W2315399125 hasConceptScore W2315399125C136764020 @default.
• W2315399125 hasConceptScore W2315399125C151730666 @default.
• W2315399125 hasConceptScore W2315399125C161191863 @default.
• W2315399125 hasConceptScore W2315399125C2778805511 @default.
• W2315399125 hasConceptScore W2315399125C2779483780 @default.
• W2315399125 hasConceptScore W2315399125C2780154274 @default.
• W2315399125 hasConceptScore W2315399125C32277403 @default.
• W2315399125 hasConceptScore W2315399125C41008148 @default.
• W2315399125 hasIssue "2" @default.
• W2315399125 hasLocation W23153991251 @default.
• W2315399125 hasOpenAccess W2315399125 @default.
• W2315399125 hasPrimaryLocation W23153991251 @default.
• W2315399125 hasRelatedWork W1534253661 @default.
• W2315399125 hasRelatedWork W1992219238 @default.
• W2315399125 hasRelatedWork W2001410255 @default.
• W2315399125 hasRelatedWork W2017614413 @default.
• W2315399125 hasRelatedWork W2041379122 @default.
• W2315399125 hasRelatedWork W2069722605 @default.
• W2315399125 hasRelatedWork W2076314280 @default.
• W2315399125 hasRelatedWork W2089427725 @default.
• W2315399125 hasRelatedWork W2097315013 @default.
• W2315399125 hasRelatedWork W2144344560 @default.
• W2315399125 hasVolume "40" @default.
• W2315399125 isParatext "false" @default.
• W2315399125 isRetracted "false" @default.
• W2315399125 magId "2315399125" @default.
• W2315399125 workType "article" @default.