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The GPS strain rate field in the Aegean Sea and western Anatolia

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dc.contributor.author Kahle, H-G en
dc.contributor.author Cocard, M en
dc.contributor.author Peter, Y en
dc.contributor.author Geiger, A en
dc.contributor.author Reilinger, R en
dc.contributor.author McClusky, S en
dc.contributor.author King, R en
dc.contributor.author Barka, A en
dc.contributor.author Veis, G en
dc.date.accessioned 2014-03-01T01:15:19Z
dc.date.available 2014-03-01T01:15:19Z
dc.date.issued 1999 en
dc.identifier.issn 0094-8276 en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/13430
dc.relation.uri http://www.scopus.com/inward/record.url?eid=2-s2.0-0033377597&partnerID=40&md5=27748fc533ad8c8c17610c32919ab9a5 en
dc.subject.classification Geosciences, Multidisciplinary en
dc.subject.other Geographical regions en
dc.subject.other Global positioning system en
dc.subject.other Interpolation en
dc.subject.other Seismology en
dc.subject.other Signal to noise ratio en
dc.subject.other Strain rate en
dc.subject.other Tectonics en
dc.subject.other Aegean sea en
dc.subject.other Seismic clusters en
dc.subject.other Tectonic faults en
dc.subject.other Western Anatolia en
dc.subject.other Geophysics en
dc.subject.other geodetic network en
dc.subject.other GPS en
dc.subject.other strain en
dc.subject.other Mediterranean Sea en
dc.subject.other Turkey en
dc.title The GPS strain rate field in the Aegean Sea and western Anatolia en
heal.type journalArticle en
heal.language English en
heal.publicationDate 1999 en
heal.abstract The GPS velocity field of the Aegean Sea and western Anatolia is used to determine crustal deformation strain rates for the period 1988 to 1996. The zone from the Marmara Sea to the North Aegean Trough is associated with strong right-lateral shear motion, with maximum strain rates of 170 nstrain/a. In the northern Aegean Sea the extensional deviatoric axes are oriented NNE-SSW, associated with strain rates reaching 150 nstrain/a, and in western Anatolia varying around N-S with rates of up to 95 nstrain/a. The extensional areas mostly coincide with active graben features. The south-western Aegean Sea is almost strain-free. In general, the areas of high geodetic strain rates are accompanied by distinct seismic clusters whereas the strain-free regions are nearly aseismic.The GPS velocity field of the Aegean Sea and western Anatolia is used to determine crustal deformation strain rates for the period 1988 to 1996. The zone from the Marmara Sea to the North Aegean Trough is associated with strong right-lateral shear motion, with maximum strain rates of 170 nstrain/a. In the northern Aegean Sea the extensional deviatoric axes are oriented NNE-SSW, associated with strain rates reaching 150 nstrain/a, and in western Anatolia varying around N-S with rates of up to 95 nstrain/a. The extensional areas mostly coincide with active graben features. The south-western Aegean Sea is almost strain-free. In general, the areas of high geodetic strain rates are accompanied by distinct seismic clusters whereas the strain-free regions are nearly aseismic. en
heal.publisher American Geophysical Union, Washington, DC, United States en
heal.journalName Geophysical Research Letters en
dc.identifier.isi ISI:000082011200027 en
dc.identifier.volume 26 en
dc.identifier.issue 16 en
dc.identifier.spage 2513 en
dc.identifier.epage 2516 en


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