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Global Positioning System constraints on plate kinematics and dynamics in the eastern Mediterranean and Caucasus

McClusky, S; Balassanian, S; Barka, A; Demir, C; Ergintav, S; Georgiev, I; Gurkan, O; Hamburger, M; Hurst, K; Kahle, H; Kastens, K; Kekelidze, G; King, R; Kotzev, V; Lenk, O; Mahmoud, S; Mishin, A; Nadariya, M; Ouzounis, A; Paradissis, D; Paradissis, D


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  <identifier identifierType="URL">https://aperta.ulakbim.gov.tr/record/93787</identifier>
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      <creatorName>McClusky, S</creatorName>
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    <creator>
      <creatorName>Balassanian, S</creatorName>
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      <familyName>Balassanian</familyName>
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      <creatorName>Barka, A</creatorName>
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      <creatorName>Demir, C</creatorName>
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      <familyName>Demir</familyName>
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      <creatorName>Ergintav, S</creatorName>
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      <familyName>Ergintav</familyName>
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      <creatorName>Georgiev, I</creatorName>
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      <familyName>Georgiev</familyName>
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      <creatorName>Gurkan, O</creatorName>
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      <creatorName>Hurst, K</creatorName>
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      <creatorName>Kahle, H</creatorName>
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      <creatorName>Kastens, K</creatorName>
      <givenName>K</givenName>
      <familyName>Kastens</familyName>
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      <creatorName>Kekelidze, G</creatorName>
      <givenName>G</givenName>
      <familyName>Kekelidze</familyName>
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      <creatorName>King, R</creatorName>
      <givenName>R</givenName>
      <familyName>King</familyName>
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    <creator>
      <creatorName>Kotzev, V</creatorName>
      <givenName>V</givenName>
      <familyName>Kotzev</familyName>
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      <creatorName>Lenk, O</creatorName>
      <givenName>O</givenName>
      <familyName>Lenk</familyName>
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      <creatorName>Mahmoud, S</creatorName>
      <givenName>S</givenName>
      <familyName>Mahmoud</familyName>
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      <creatorName>Mishin, A</creatorName>
      <givenName>A</givenName>
      <familyName>Mishin</familyName>
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      <creatorName>Nadariya, M</creatorName>
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      <creatorName>Ouzounis, A</creatorName>
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      <creatorName>Paradissis, D</creatorName>
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      <creatorName>Paradissis, D</creatorName>
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  <titles>
    <title>Global Positioning System Constraints On Plate Kinematics And Dynamics In The Eastern Mediterranean And Caucasus</title>
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  <publisher>Aperta</publisher>
  <publicationYear>2000</publicationYear>
  <dates>
    <date dateType="Issued">2000-01-01</date>
  </dates>
  <resourceType resourceTypeGeneral="Text">Journal article</resourceType>
  <alternateIdentifiers>
    <alternateIdentifier alternateIdentifierType="url">https://aperta.ulakbim.gov.tr/record/93787</alternateIdentifier>
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    <relatedIdentifier relatedIdentifierType="DOI" relationType="IsVersionOf">10.81043/aperta.93786</relatedIdentifier>
    <relatedIdentifier relatedIdentifierType="DOI" relationType="IsIdenticalTo">10.81043/aperta.93787</relatedIdentifier>
  </relatedIdentifiers>
  <rightsList>
    <rights rightsURI="http://www.opendefinition.org/licenses/cc-by">Creative Commons Attribution</rights>
    <rights rightsURI="info:eu-repo/semantics/openAccess">Open Access</rights>
  </rightsList>
  <descriptions>
    <description descriptionType="Abstract">We present and interpret Global Positioning System (GPS) measurements of crustal motions for the period 1988-1997 at 189 sites extending east-west from the Caucasus mountains to the Adriatic Sea and north-south from the southern edge of the Eurasian plate to the northern edge of the African plate. Sites on the northern Arabian platform move 18 +/- 2 mm/yr at N25 degrees +/- 5 degrees W relative to Eurasia, less than the NUVEL-1A circuit closure rate (25 +/- 1 mm/yr at N21 degrees +/- 7 degrees W). Preliminary motion estimates (1994-1997) for stations located in Egypt on the northeastern part of Africa show northward motion at 5-6 +/- 2 mm/yr, also slower than NUVEL-1A estimates (10 +/- 1 mm/yr at N2 degrees +/- 4 degrees E). Eastern Turkey is characterized by distributed deformation, while central Turkey is characterized by coherent plate motion (internal deformation of &amp;lt;2 mm/yr) involving westward displacement and counterclockwise rotation of the Anatolian plate. The Anatolian plate is de-coupled from Eurasia along the right-lateral, strike-slip North Anatolian fault (NAF). We derive a best fitting Euler vector for Anatolia-Eurasia motion of 30.7 degrees +/- 0.8 degrees N, 32.6 degrees +/- 0.4 degrees E, 1.2 degrees +/- 0.1 degrees/Myr. The Euler vector gives an upper bound for NAF slip rate of 24 +/- 1 mm/yr. We determine a preliminary GPS Arabia-Anatolia Euler vector of 32.9 degrees +/- 1.2 degrees N, 40.3 degrees +/- 1.1 degrees E, 0.8 degrees +/- 0.2 degrees/Myr and an upper bound on left-lateral slip on the East Anatolian fault (EAF) of 9 +/- 1 mm/yr. The central, and southern Aegean is characterized by coherent motion (internal deformation of &amp;lt;2 mm/yr) toward the SW at 30 +/- 1 mm/yr relative to Eurasia. Stations in the SE aegean deviate significantly from the overall motion of the southern Aegean, showing increasing velocities toward the trench and reaching 10 +/- 1 mm/yr relative to the southern Aegean as a whole.</description>
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