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The viscosity of Earth's lower mantle inferred from sinking speed of subducted lithosphere

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11320%2F12%3A10123581" target="_blank" >RIV/00216208:11320/12:10123581 - isvavai.cz</a>

  • Result on the web

    <a href="http://dx.doi.org/10.1016/j.pepi.2012.02.010" target="_blank" >http://dx.doi.org/10.1016/j.pepi.2012.02.010</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.pepi.2012.02.010" target="_blank" >10.1016/j.pepi.2012.02.010</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    The viscosity of Earth's lower mantle inferred from sinking speed of subducted lithosphere

  • Original language description

    The viscosity of the mantle is indispensable for predicting Earth''s mechanical behavior at scales ranging from deep mantle material flow to local stress accumulation in earthquakes zones. But, mantle viscosity is not well determined. For the lower mantle, particularly, only few constraints result from elaborate high-pressure experiments (Karato, 2008) and a variety of viscosity depth profiles result from joint inversion of the geoid and postglacial rebound data (Forte and Mitrovica, 1996; Kaufmann andLambeck, 2000; Mitrovica and Forte, 2004). Here, we use inferred lower-mantle sinking speed of lithosphere subduction remnants as a unique internal constraint on modeling the viscosity profile. This entails a series of elaborate dynamic subduction calculations spanning a range of viscosity profiles from which we select profiles that predict the inferred sinking speed of 12 +/- 3 mm/yr (van der Meer et al., 2010). Our modeling shows that sinking speed is very sensitive to lower mantle vis

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

  • CEP classification

    DE - Earth magnetism, geodesy, geography

  • OECD FORD branch

Result continuities

  • Project

    <a href="/en/project/GAP210%2F11%2F1366" target="_blank" >GAP210/11/1366: Transport Properties and Dynamics of the Earth's Lower Mantle</a><br>

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>Z - Vyzkumny zamer (s odkazem do CEZ)

Others

  • Publication year

    2012

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    PHYSICS OF THE EARTH AND PLANETARY INTERIORS

  • ISSN

    0031-9201

  • e-ISSN

  • Volume of the periodical

    200

  • Issue of the periodical within the volume

    6

  • Country of publishing house

    NL - THE KINGDOM OF THE NETHERLANDS

  • Number of pages

    7

  • Pages from-to

    56-62

  • UT code for WoS article

    000306047200006

  • EID of the result in the Scopus database