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New geodetic constraints on the role of faults and blocks versus distributed strain in the Nubia-Arabia-Eurasia zone of active plate interactions

Ergintav Semih; Floyd Michael; Paradissis Demitris; Karabulut Hayrullah; Vernant Philippe; Mason Frederic; Ivan Georgiev; Ali Özgün Konca; Uğur Doğan; Robert King; Robert Reilienger


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    <subfield code="a">&lt;p&gt;Contents This supporting information contains supplementary figures and information about the tables, presented and discussed in the text. Figure S1 shows the slip rates along block model boundaries. Figure S2 demonstrates the variations of locking depths along the North Anatolian Fault, with a series of fault perpendicular profiles. Figure S3 shows that the model residuals south of the western NAF are associated with deep, ongoing postseismic effects of the 1999 Izmit/D&amp;uuml;zce earthquake sequence. Table S1 (&amp;#39;full_velocity_05052022.txt.zip&amp;#39;) show the present velocity files with respect to Aegean, Anatolia and East Anatolia. Reference sites marked with R1, R2, R3, for Aegean, Anatolia and East Anatolia, respectively. Table S2 (&amp;#39;fault_rates_05052022.pdf&amp;#39;) includes the GNSS derived fault slip rates deduced from the block model. These tables are uploaded, separately.&lt;/p&gt;</subfield>
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    <subfield code="u">MIT, ABD</subfield>
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    <subfield code="u">National Technical University of Athens, Athens, yunanistan</subfield>
    <subfield code="a">Paradissis Demitris</subfield>
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    <subfield code="u">Bogazici Universitesi, İstanbul</subfield>
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    <subfield code="u">University of Montpellier, Montpellier, France</subfield>
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    <subfield code="u">Yıldız Technical University, Istanbul, Turkey</subfield>
    <subfield code="a">Uğur Doğan</subfield>
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