Morphology of the wadati-benioff zone in the hellenic arc
Identifieur interne : 000168 ( Istex/Corpus ); précédent : 000167; suivant : 000169Morphology of the wadati-benioff zone in the hellenic arc
Auteurs : J. Van K ; V. Hanuš ; C. Christova ; S. SimeonovaSource :
- Journal of Geodynamics [ 0264-3707 ] ; 1987.
English descriptors
- KwdEn :
- Active volcanism, Active volcanoes, Adjacent areas, Aegean area, Aegean region, Aseismic, Average subduction rate, Christova, Earthquake foci, Eastern part, Fracture, Fracture zone, Fracture zones, Hanug, Hellenic subduction zone, Hellenic trench, Lower limit, Maximum depth, Morphology, Overlying wedge, Seismically, Subduction, Subduction zone, Tectonophysics, Trench, Trench axis, Van6k, Vertical sections, Volcanism, Volcano, Western part, Western turkey, Zone.
- Teeft :
- Active volcanism, Active volcanoes, Adjacent areas, Aegean area, Aegean region, Aseismic, Average subduction rate, Christova, Earthquake foci, Eastern part, Fracture, Fracture zone, Fracture zones, Hanug, Hellenic subduction zone, Hellenic trench, Lower limit, Maximum depth, Morphology, Overlying wedge, Seismically, Subduction, Subduction zone, Tectonophysics, Trench, Trench axis, Van6k, Vertical sections, Volcanism, Volcano, Western part, Western turkey, Zone.
Abstract
Abstract: The morphology of the Wadati-Benioff zone in the Hellenic arc was established on the basis of the distribution of 1058 earthquake foci. The subduction zone appears to be composed of two separated parts (western and eastern) terminated by seismically active fracture zones. The existence of an intermediate depth aseismic gap, closely connected with active calc-alkaline volcanism, was confirmed in both parts. The age and the average subduction rate of the present subduction cycle were estimated.
Url:
DOI: 10.1016/0264-3707(87)90059-7
Links to Exploration step
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<front><div type="abstract" xml:lang="en">Abstract: The morphology of the Wadati-Benioff zone in the Hellenic arc was established on the basis of the distribution of 1058 earthquake foci. The subduction zone appears to be composed of two separated parts (western and eastern) terminated by seismically active fracture zones. The existence of an intermediate depth aseismic gap, closely connected with active calc-alkaline volcanism, was confirmed in both parts. The age and the average subduction rate of the present subduction cycle were estimated.</div>
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<ce:abstract-sec><ce:simple-para>The morphology of the Wadati-Benioff zone in the Hellenic arc was established on the basis of the distribution of 1058 earthquake foci. The subduction zone appears to be composed of two separated parts (western and eastern) terminated by seismically active fracture zones. The existence of an intermediate depth aseismic gap, closely connected with active calc-alkaline volcanism, was confirmed in both parts. The age and the average subduction rate of the present subduction cycle were estimated.</ce:simple-para>
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