On the possibility of a steady state backflow in the mantle wedge

Result code in IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11320%2F09%3A00206517" target="_blank" >RIV/00216208:11320/09:00206517 - isvavai.cz</a>

Result on the web

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DOI - Digital Object Identifier

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Result language

angličtina

Original language name

On the possibility of a steady state backflow in the mantle wedge

Original language description

We developed a numerical model of a pseudo-plastic subduction plate. The results showed that both the temperature field and the geometry of the slab are strongly controlled by weakness zones in the topmost part of the subducting plate and in the cold tipof the mantle wedge. We showed that a backward flow may evolve along the plate wedge interface if the cold portion of the mantle wedge is weak

Czech name

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Czech description

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Type

J_x - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

CEP classification

DE - Earth magnetism, geodesy, geography

OECD FORD branch

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Project

<a href="/en/project/GA205%2F09%2F0546" target="_blank" >GA205/09/0546: Reconciling present-day and long-term ice-mass variations resolved from satellite observations with glacial-isostatic-adjustment models</a><br>

Continuities

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

Publication year

2009

Confidentiality

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

Name of the periodical

Geophysical Journal International

ISSN

0956-540X

e-ISSN

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Volume of the periodical

177

Issue of the periodical within the volume

1

Country of publishing house

GB - UNITED KINGDOM

Number of pages

7

Pages from-to

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UT code for WoS article

000266025200031

EID of the result in the Scopus database

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