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  • Cratons with their thick lithospheric roots can influence the thermal structure, and thus the convective flow, in the surrounding mantle. As mantle temperatures are hard to measure directly, depth variations in the mantle transition zone (MTZ) discontinuities are often employed as a proxy. Here, we use a large new data set of P-receiver functions to map the 410 km and 660 km discontinuities beneath the western edge of the East European Craton and adjacent Phanerozoic Europe across the most fundamental lithospheric boundary in Europe, the Trans-European Suture Zone (TESZ). We observe significantly shorter travel times for conversions from both MTZ discontinuities within the craton, caused by the high velocities of the cratonic root.
  • Cratons with their thick lithospheric roots can influence the thermal structure, and thus the convective flow, in the surrounding mantle. As mantle temperatures are hard to measure directly, depth variations in the mantle transition zone (MTZ) discontinuities are often employed as a proxy. Here, we use a large new data set of P-receiver functions to map the 410 km and 660 km discontinuities beneath the western edge of the East European Craton and adjacent Phanerozoic Europe across the most fundamental lithospheric boundary in Europe, the Trans-European Suture Zone (TESZ). We observe significantly shorter travel times for conversions from both MTZ discontinuities within the craton, caused by the high velocities of the cratonic root. (en)
Title
  • Tracing the influence of the Trans-European Suture Zone into the mantle transition zone
  • Tracing the influence of the Trans-European Suture Zone into the mantle transition zone (en)
skos:prefLabel
  • Tracing the influence of the Trans-European Suture Zone into the mantle transition zone
  • Tracing the influence of the Trans-European Suture Zone into the mantle transition zone (en)
skos:notation
  • RIV/67985530:_____/13:00422858!RIV14-AV0-67985530
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • I
http://linked.open...iv/cisloPeriodika
  • FEB 1
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
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http://linked.open...dnocenehoVysledku
  • 111458
http://linked.open...ai/riv/idVysledku
  • RIV/67985530:_____/13:00422858
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • mantle transition zone; Trans-European Suture Zone; East European Craton (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • NL - Nizozemsko
http://linked.open...ontrolniKodProRIV
  • [AE58D114995E]
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  • Earth and Planetary Science Letters
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http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 363
http://linked.open...iv/tvurceVysledku
  • Málek, Jiří
  • Novotný, Oldřich
  • Gaždová, Renata
  • Jedlička, Petr
  • Babuška, Vladislav
  • Plomerová, Jaroslava
  • Kolínský, Petr
  • Růžek, Bohuslav
  • Geissler, W. H.
  • Knapmeyer-Endrun, B.
  • Krüger, F.
  • Legendre, C. P.
http://linked.open...ain/vavai/riv/wos
  • 000316643300009
issn
  • 0012-821X
number of pages
http://bibframe.org/vocab/doi
  • 10.1016/j.epsl.2012.12.028
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