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Mantle dynamics beneath Greece from SKS and PKS seismic anisotropy study

Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
SKS and PKS splitting parameters were determined in the broader Greek region using data from 45 stations of the Hellenic Unified Seismological Network and the Kandilli Observatory and Earthquake Research Institute, utilizing teleseismic events that occurred between 2010 and 2017. Data were processed for shear-wave splitting with the Minimum Energy Method that was considered the optimal. The results generally confirm the existence of anisotropic zonation in the Hellenic subduction system, with alternating trench-normal and trench-parallel directions. The zonation is attributed to the upper and lower olivine fabric layers that can, potentially, be present in the subduction zone. At the edges of this zone, two possible toroidal flow cases have been identified, implying the existence of tears that allow the inflow of asthenospheric material in the mantle wedge. The high number of null measurements in the KZN and XOR stations indicates a possible anisotropic transition zone between the fore-arc and back-arc areas. SKS and PKS splitting results are jointly interpreted, given that they yield similar values in most cases.
Czasopismo
Rocznik
Strony
1341--1357
Opis fizyczny
Bibliogr. 100 poz.
Twórcy
autor
  • Section of Geophysics and Geothermics, Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, Panepistimiopolis, Zografou, 157 84 Athens, Greece, gkaviris@geol.uoa.gr
  • Section of Geophysics and Geothermics, Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, Panepistimiopolis, Zografou, 157 84 Athens, Greece
autor
  • Section of Geophysics and Geothermics, Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, Panepistimiopolis, Zografou, 157 84 Athens, Greece
autor
  • Section of Geophysics and Geothermics, Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, Panepistimiopolis, Zografou, 157 84 Athens, Greece
  • Section of Geophysics and Geothermics, Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, Panepistimiopolis, Zografou, 157 84 Athens, Greece
autor
  • Geodynamic Institute, National Observatory of Athens, Lofos Nymfon, Thission, 11810 Athens, Greece
Bibliografia
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Uwagi
Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2019).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-140e8379-c594-457c-ab48-13a5d9a5f340
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