1 Ocak 2020 Dergi makalesi Açık Erişim

Aydin, Faruk; Saka, Simge Oguz; Sen, Cuneyt; Dokuz, Abdurrahman; Aiglsperger, Thomas; Uysal, Ibrahim; Kandemir, Raif; Karsli, Orhan; San, Bilal; Baser, Rasim

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  <identifier identifierType="URL">https://aperta.ulakbim.gov.tr/record/6139</identifier>
  <creators>
    <creator>
      <creatorName>Aydin, Faruk</creatorName>
      <givenName>Faruk</givenName>
      <familyName>Aydin</familyName>
      <affiliation>Karadeniz Tech Univ, Dept Geol Engn, Trabzon, Turkey</affiliation>
    </creator>
    <creator>
      <creatorName>Saka, Simge Oguz</creatorName>
      <givenName>Simge Oguz</givenName>
      <familyName>Saka</familyName>
      <affiliation>Karadeniz Tech Univ, Dept Geol Engn, Trabzon, Turkey</affiliation>
    </creator>
    <creator>
      <creatorName>Sen, Cuneyt</creatorName>
      <givenName>Cuneyt</givenName>
      <familyName>Sen</familyName>
      <affiliation>Karadeniz Tech Univ, Dept Geol Engn, Trabzon, Turkey</affiliation>
    </creator>
    <creator>
      <creatorName>Dokuz, Abdurrahman</creatorName>
      <givenName>Abdurrahman</givenName>
      <familyName>Dokuz</familyName>
      <affiliation>Gumushane Univ, Dept Geol Engn, Gumushane, Turkey</affiliation>
    </creator>
    <creator>
      <creatorName>Aiglsperger, Thomas</creatorName>
      <givenName>Thomas</givenName>
      <familyName>Aiglsperger</familyName>
      <affiliation>Lulea Univ Technol, Dept Civil Engn &amp; Nat Resources, Div Geosci &amp; Environm Engn, Lulea, Sweden</affiliation>
    </creator>
    <creator>
      <creatorName>Uysal, Ibrahim</creatorName>
      <givenName>Ibrahim</givenName>
      <familyName>Uysal</familyName>
      <affiliation>Karadeniz Tech Univ, Dept Geol Engn, Trabzon, Turkey</affiliation>
    </creator>
    <creator>
      <creatorName>Kandemir, Raif</creatorName>
      <givenName>Raif</givenName>
      <familyName>Kandemir</familyName>
      <affiliation>Recep Tayyip Erdogan Univ, Dept Geol Engn, Rize, Turkey</affiliation>
    </creator>
    <creator>
      <creatorName>Karsli, Orhan</creatorName>
      <givenName>Orhan</givenName>
      <familyName>Karsli</familyName>
      <affiliation>Recep Tayyip Erdogan Univ, Dept Geol Engn, Rize, Turkey</affiliation>
    </creator>
    <creator>
      <creatorName>San, Bilal</creatorName>
      <givenName>Bilal</givenName>
      <familyName>San</familyName>
      <affiliation>Dokuz Eylul Univ, Dept Geol Engn, Izmir, Turkey</affiliation>
    </creator>
    <creator>
      <creatorName>Baser, Rasim</creatorName>
      <givenName>Rasim</givenName>
      <familyName>Baser</familyName>
      <affiliation>Karadeniz Tech Univ, Dept Geol Engn, Trabzon, Turkey</affiliation>
    </creator>
  </creators>
  <titles>
    <title>Temporal, Geochemical And Geodynamic Evolution Of The Late Cretaceous Subduction Zone Volcanism In The Eastern Sakarya Zone, Ne Turkey: Implications For Mantle-Crust Interaction In An Arc Setting</title>
  </titles>
  <publisher>Aperta</publisher>
  <publicationYear>2020</publicationYear>
  <dates>
    <date dateType="Issued">2020-01-01</date>
  </dates>
  <resourceType resourceTypeGeneral="Text">Journal article</resourceType>
  <alternateIdentifiers>
    <alternateIdentifier alternateIdentifierType="url">https://aperta.ulakbim.gov.tr/record/6139</alternateIdentifier>
  </alternateIdentifiers>
  <relatedIdentifiers>
    <relatedIdentifier relatedIdentifierType="DOI" relationType="IsIdenticalTo">10.1016/j.jseaes.2019.104217</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">The Late Cretaceous Artvin volcanic rocks (LCAVs) from the eastern Sakarya zone (ESZ) of NE Turkey are composed of mafic/basaltic (S1-catak and S2-caglayan) and felsic/acidic (S1-Kizilkaya and S2-Tirebolu) rock types that occurred in two successive stages: (i) first stage (S1: Turonian-Early Santonian) and (ii) second stage (S2: Late Santonian-Campanian). Clinopyroxene thermobarometric results point that the S2-caglayan basaltic rocks have crystallised at higher temperatures and under deeper crustal conditions than those of the S1-catak basaltic rocks.</description>
  </descriptions>
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