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- W2124173619 abstract "Research Article| May 01, 2008 How warm are passive continental margins? A 3-D lithosphere-scale study from the Norwegian margin Magdalena Scheck-Wenderoth; Magdalena Scheck-Wenderoth * 1GeoForschungsZentrum Potsdam in der Helmholtz Gemeinschaft, Telegrafenberg, 14473 Potsdam, Germany *E-mail:leni@gfz-potsdam.de. Search for other works by this author on: GSW Google Scholar Yuriy Maystrenko Yuriy Maystrenko 1GeoForschungsZentrum Potsdam in der Helmholtz Gemeinschaft, Telegrafenberg, 14473 Potsdam, Germany Search for other works by this author on: GSW Google Scholar Geology (2008) 36 (5): 419–422. https://doi.org/10.1130/G24545A.1 Article history received: 02 Nov 2007 rev-recd: 28 Jan 2008 accepted: 06 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 Magdalena Scheck-Wenderoth, Yuriy Maystrenko; How warm are passive continental margins? A 3-D lithosphere-scale study from the Norwegian margin. Geology 2008;; 36 (5): 419–422. doi: https://doi.org/10.1130/G24545A.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 We model the three-dimensional (3-D) conductive thermal field of the Norwegian margin and evaluate its lithospheric configuration, which is consistent with two independent observables: temperature and gravity. Here, we show that knowledge of the sediment and crustal configuration of the passive continental margin provides constraints for the configuration and thermal structure of the lithosphere. We find that the thickness of the oceanic lithosphere adjacent to the stretched continental margin controls, to a large degree, the shallow conductive thermal field of the entire margin. Our results confirm estimates of lithospheric thickness from seismology but contradict estimates from cooling models, which assume an equilibrium thickness of the oceanic lithosphere of 125 km. We find that the crust is colder in the oceanic than in the continental domain, whereas this trend is reversed downward. We obtain lateral temperature differences of ~100 °C at 5 km depth across the margin that increase to ~400 °C at 50 km depth. Higher temperatures and heat flows for the oceanic lithospheric mantle compared to the continent indicate that reduced upper-mantle P-wave velocities and densities are thermally induced. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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- W2124173619 title "How warm are passive continental margins? A 3-D lithosphere-scale study from the Norwegian margin" @default.
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