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Influence of Variable Thermal Expansivity and Conductivity on Deep Subduction

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F15%3A00000185" target="_blank" >RIV/00025798:_____/15:00000185 - isvavai.cz</a>

  • Result on the web

    <a href="http://eu.wiley.com/WileyCDA/WileyTitle/productCd-1118888855.html" target="_blank" >http://eu.wiley.com/WileyCDA/WileyTitle/productCd-1118888855.html</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1002/9781118888865.ch0" target="_blank" >10.1002/9781118888865.ch0</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Influence of Variable Thermal Expansivity and Conductivity on Deep Subduction

  • Original language description

    Thickening of slabs subducted in the lower mantle is a robust feature from seismic tomography. Numerical models show clearly that, under suitable circumstances, deeply subducted plates experience buckling instabilities near the transition zone. These canlead to the formation of large-scale folds, which ultimately cause the lower mantle portion of slabs to be significantly thicker than the upper mantle part. Such models, however, generally rely on the assumption of constant thermodynamic properties. Here we present subduction simulations that include pressure-, temperature-, and phase-dependent thermal expansivity and conductivity, and demonstrate that these parameters exert a dramatic effect on the dynamics of lower mantle slabs. The decrease of expansivity with pressure causes slabs to lose buoyancy during their descent. This strongly enhances buckling and reduces sinking speed, thereby promoting thermal diffusion and a significant spreading of the slab thermal anomalies in the lower

  • Czech name

  • Czech description

Classification

  • Type

    C - Chapter in a specialist book

  • CEP classification

    DB - Geology and mineralogy

  • OECD FORD branch

Result continuities

  • Project

    <a href="/en/project/LK11202" target="_blank" >LK11202: The role of Paleozoic accretionary and collisanal orogens on the formation and growth of continental crust</a><br>

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Others

  • Publication year

    2015

  • Confidentiality

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

Data specific for result type

  • Book/collection name

    Subduction Dynamics: From Mantle Flow to Mega Disasters

  • ISBN

    9781118888858

  • Number of pages of the result

    19

  • Pages from-to

    115-133

  • Number of pages of the book

    210

  • Publisher name

    American Geophysical Union

  • Place of publication

    Washington

  • UT code for WoS chapter