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.

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        "affiliation": "Dokuz Eylul Univ, Muhendisl Fak, Jeol Muh Bol, Buca Izmir, Turkey", 
        "name": "Candan, O."
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      {
        "affiliation": "Dokuz Eylul Univ, Muhendisl Fak, Jeol Muh Bol, Buca Izmir, Turkey", 
        "name": "Koralay, O. E."
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      {
        "affiliation": "Dokuz Eylul Univ, Muhendisl Fak, Jeol Muh Bol, Buca Izmir, Turkey", 
        "name": "Akal, C."
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      {
        "affiliation": "Dokuz Eylul Univ, Muhendisl Fak, Jeol Muh Bol, Bornova, Turkey", 
        "name": "Kaya, O."
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      {
        "affiliation": "Univ Potsdam, Inst Erd & Umweltwissensch, D-14476 Potsdam, Germany", 
        "name": "Oberhansli, R."
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      {
        "affiliation": "Dokuz Eylul Univ, Muhendisl Fak, Jeol Muh Bol, Buca Izmir, Turkey", 
        "name": "Dora, O. O."
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      {
        "affiliation": "Maden Tetk & Arama Genel Mudurlugu, Jeol Araltirmalari Birimi, Cankaya, Turkey", 
        "name": "Konak, N."
      }, 
      {
        "affiliation": "Univ Sci & Technol China, Chinese Acad Sci, Key Lab Crust Mantle Mat & Environm, Hefei 230026, Peoples R China", 
        "name": "Chen, F."
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    "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.", 
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    "journal": {
      "issue": "1-4", 
      "pages": "1-23", 
      "title": "PRECAMBRIAN RESEARCH", 
      "volume": "184"
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      "title": "Dergi makalesi", 
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    "title": "Supra-Pan-African unconformity between core and cover series of the Menderes Massif/Turkey and its geological implications"
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