Morphology of the wadati-benioff zone in the hellenic arc
Identifieur interne : 000461 ( Main/Exploration ); précédent : 000460; suivant : 000462Morphology of the wadati-benioff zone in the hellenic arc
Auteurs : J. Van K [Tchécoslovaquie] ; V. Hanuš [Tchécoslovaquie] ; C. Christova [Bulgarie] ; S. Simeonova [Bulgarie]Source :
- 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
Affiliations:
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Sci., 1113 Sofia</wicri:regionArea><placeName><settlement type="city">Sofia</settlement><region nuts="2">Sofia-ville (oblast)</region></placeName></affiliation></author></analytic><monogr></monogr><series><title level="j">Journal of Geodynamics</title><title level="j" type="abbrev">GEOD</title><idno type="ISSN">0264-3707</idno><imprint><publisher>ELSEVIER</publisher><date type="published" when="1987">1987</date><biblScope unit="volume">8</biblScope><biblScope unit="issue">1</biblScope><biblScope unit="page" from="79">79</biblScope><biblScope unit="page" to="93">93</biblScope></imprint><idno type="ISSN">0264-3707</idno></series></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0264-3707</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Active volcanism</term><term>Active volcanoes</term><term>Adjacent areas</term><term>Aegean area</term><term>Aegean region</term><term>Aseismic</term><term>Average subduction rate</term><term>Christova</term><term>Earthquake foci</term><term>Eastern part</term><term>Fracture</term><term>Fracture zone</term><term>Fracture zones</term><term>Hanug</term><term>Hellenic subduction zone</term><term>Hellenic trench</term><term>Lower limit</term><term>Maximum depth</term><term>Morphology</term><term>Overlying wedge</term><term>Seismically</term><term>Subduction</term><term>Subduction zone</term><term>Tectonophysics</term><term>Trench</term><term>Trench axis</term><term>Van6k</term><term>Vertical sections</term><term>Volcanism</term><term>Volcano</term><term>Western part</term><term>Western turkey</term><term>Zone</term></keywords><keywords scheme="Teeft" xml:lang="en"><term>Active volcanism</term><term>Active volcanoes</term><term>Adjacent areas</term><term>Aegean area</term><term>Aegean region</term><term>Aseismic</term><term>Average subduction rate</term><term>Christova</term><term>Earthquake foci</term><term>Eastern part</term><term>Fracture</term><term>Fracture zone</term><term>Fracture zones</term><term>Hanug</term><term>Hellenic subduction zone</term><term>Hellenic trench</term><term>Lower limit</term><term>Maximum depth</term><term>Morphology</term><term>Overlying wedge</term><term>Seismically</term><term>Subduction</term><term>Subduction zone</term><term>Tectonophysics</term><term>Trench</term><term>Trench axis</term><term>Van6k</term><term>Vertical sections</term><term>Volcanism</term><term>Volcano</term><term>Western part</term><term>Western turkey</term><term>Zone</term></keywords></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><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></front></TEI><affiliations><list><country><li>Bulgarie</li><li>Tchécoslovaquie</li></country><region><li>Sofia-ville (oblast)</li></region><settlement><li>Sofia</li></settlement></list><tree><country name="Tchécoslovaquie"><noRegion><name sortKey="Van K, J" sort="Van K, J" uniqKey="Van K J" first="J." last="Van K">J. Van K</name></noRegion><name sortKey="Hanus, V" sort="Hanus, V" uniqKey="Hanus V" first="V." last="Hanuš">V. Hanuš</name></country><country name="Bulgarie"><region name="Sofia-ville (oblast)"><name sortKey="Christova, C" sort="Christova, C" uniqKey="Christova C" first="C." last="Christova">C. Christova</name></region><name sortKey="Simeonova, S" sort="Simeonova, S" uniqKey="Simeonova S" first="S." last="Simeonova">S. Simeonova</name></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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