Dergi makalesi Açık Erişim
Candan, O.; Koralay, O. E.; Akal, C.; Kaya, O.; Oberhansli, R.; Dora, O. O.; Konak, N.; Chen, F.
<?xml version='1.0' encoding='UTF-8'?> <record xmlns="http://www.loc.gov/MARC21/slim"> <leader>00000nam##2200000uu#4500</leader> <datafield tag="700" ind1=" " ind2=" "> <subfield code="a">Koralay, O. E.</subfield> <subfield code="u">Dokuz Eylul Univ, Muhendisl Fak, Jeol Muh Bol, Buca Izmir, Turkey</subfield> </datafield> <datafield tag="700" ind1=" " ind2=" "> <subfield code="a">Akal, C.</subfield> <subfield code="u">Dokuz Eylul Univ, Muhendisl Fak, Jeol Muh Bol, Buca Izmir, Turkey</subfield> </datafield> <datafield tag="700" ind1=" " ind2=" "> <subfield code="a">Kaya, O.</subfield> <subfield code="u">Dokuz Eylul Univ, Muhendisl Fak, Jeol Muh Bol, Bornova, Turkey</subfield> </datafield> <datafield tag="700" ind1=" " ind2=" "> <subfield code="a">Oberhansli, R.</subfield> <subfield code="u">Univ Potsdam, Inst Erd & Umweltwissensch, D-14476 Potsdam, Germany</subfield> </datafield> <datafield tag="700" ind1=" " ind2=" "> <subfield code="a">Dora, O. O.</subfield> <subfield code="u">Dokuz Eylul Univ, Muhendisl Fak, Jeol Muh Bol, Buca Izmir, Turkey</subfield> </datafield> <datafield tag="700" ind1=" " ind2=" "> <subfield code="a">Konak, N.</subfield> <subfield code="u">Maden Tetk & Arama Genel Mudurlugu, Jeol Araltirmalari Birimi, Cankaya, Turkey</subfield> </datafield> <datafield tag="700" ind1=" " ind2=" "> <subfield code="a">Chen, F.</subfield> <subfield code="u">Univ Sci & Technol China, Chinese Acad Sci, Key Lab Crust Mantle Mat & Environm, Hefei 230026, Peoples R China</subfield> </datafield> <datafield tag="909" ind1="C" ind2="4"> <subfield code="p">PRECAMBRIAN RESEARCH</subfield> <subfield code="v">184</subfield> <subfield code="n">1-4</subfield> <subfield code="c">1-23</subfield> </datafield> <datafield tag="980" ind1=" " ind2=" "> <subfield code="a">user-tubitak-destekli-proje-yayinlari</subfield> </datafield> <datafield tag="540" ind1=" " ind2=" "> <subfield code="a">Creative Commons Attribution</subfield> <subfield code="u">http://www.opendefinition.org/licenses/cc-by</subfield> </datafield> <datafield tag="024" ind1=" " ind2=" "> <subfield code="a">10.1016/j.precamres.2010.09.010</subfield> <subfield code="2">doi</subfield> </datafield> <datafield tag="245" ind1=" " ind2=" "> <subfield code="a">Supra-Pan-African unconformity between core and cover series of the Menderes Massif/Turkey and its geological implications</subfield> </datafield> <datafield tag="100" ind1=" " ind2=" "> <subfield code="a">Candan, O.</subfield> <subfield code="u">Dokuz Eylul Univ, Muhendisl Fak, Jeol Muh Bol, Buca Izmir, Turkey</subfield> </datafield> <datafield tag="909" ind1="C" ind2="O"> <subfield code="o">oai:zenodo.org:18591</subfield> <subfield code="p">user-tubitak-destekli-proje-yayinlari</subfield> </datafield> <datafield tag="650" ind1="1" ind2="7"> <subfield code="2">opendefinition.org</subfield> <subfield code="a">cc-by</subfield> </datafield> <datafield tag="260" ind1=" " ind2=" "> <subfield code="c">2011-01-01</subfield> </datafield> <datafield tag="856" ind1="4" ind2=" "> <subfield code="u">https://aperta.ulakbim.gov.trrecord/18591/files/bib-bf9cfd25-89e9-44b5-af17-13692f631743.txt</subfield> <subfield code="z">md5:bbd5ab6c4360a8643fcb8cd31f8ad0c9</subfield> <subfield code="s">261</subfield> </datafield> <datafield tag="542" ind1=" " ind2=" "> <subfield code="l">open</subfield> </datafield> <controlfield tag="005">20210315101021.0</controlfield> <controlfield tag="001">18591</controlfield> <datafield tag="980" ind1=" " ind2=" "> <subfield code="a">publication</subfield> <subfield code="b">article</subfield> </datafield> <datafield tag="520" ind1=" " ind2=" "> <subfield code="a">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.</subfield> </datafield> </record>
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