1 Ocak 2011 Dergi makalesi Açık Erişim

Candan, O.; Koralay, O. E.; Akal, C.; Kaya, O.; Oberhansli, R.; Dora, O. O.; Konak, N.; Chen, F.

Dublin Core

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  <dc:creator>Candan, O.</dc:creator>
  <dc:creator>Koralay, O. E.</dc:creator>
  <dc:creator>Akal, C.</dc:creator>
  <dc:creator>Kaya, O.</dc:creator>
  <dc:creator>Oberhansli, R.</dc:creator>
  <dc:creator>Dora, O. O.</dc:creator>
  <dc:creator>Konak, N.</dc:creator>
  <dc:creator>Chen, F.</dc:creator>
  <dc:date>2011-01-01</dc:date>
  <dc:description>Well-preserved primary contact relationships between a Late Proterozoic metasedimentary and the metagranitic core and Palaeozoic cover series of the Menderes Massif have been recognized in the eastern part of the Cine submassif on a regional-scale. Metaconglomerates occur as laterally discontinuous channel-fill bodies close the base of the metaquartzarenite directly above the basement. The pebbles in the metaconglomerates consist mainly of different types of tourmaline-rich leucocratic granitoids, tourmalinite and schist in a sandy matrix. Petrographic features, geochemical compositions and zircon radiometric ages (549.6 +/- 3.7-552.3 +/- 3.1 Ma) of the diagnostic clasts of the metaconglomerates (e.g. leucocratic granitoids and tourmalinites) show excellent agreement with their in situ equivalents (549.0 +/- 5.4 Ma) occurring in the Pan-African basement as stocks and veins.</dc:description>
  <dc:identifier>https://aperta.ulakbim.gov.trrecord/18591</dc:identifier>
  <dc:identifier>oai:zenodo.org:18591</dc:identifier>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>http://www.opendefinition.org/licenses/cc-by</dc:rights>
  <dc:source>PRECAMBRIAN RESEARCH 184(1-4) 1-23</dc:source>
  <dc:title>Supra-Pan-African unconformity between core and cover series of the Menderes Massif/Turkey and its geological implications</dc:title>
  <dc:type>info:eu-repo/semantics/article</dc:type>
  <dc:type>publication-article</dc:type>
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