1 Ocak 2019 Konferans bildirisi Açık Erişim

Ozyurt, Merve; Al-Aasm, Ihsan S.; Kirmaci, M. Ziya

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    "creators": [
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        "name": "Ozyurt, Merve"
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      {
        "affiliation": "Univ Windsor, Dept Earth & Environm Sci, 401 Sunset Ave, Windsor, ON N9B 3P4, Canada", 
        "name": "Al-Aasm, Ihsan S."
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      {
        "affiliation": "Karadeniz Tech Univ, Dept Geol Engn, TR-61080 Trabzon, Turkey", 
        "name": "Kirmaci, M. Ziya"
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    "description": "Upper Jurassic-lower Cretaceous Berdiga Formation crops out extensively in NE Turkey. The host carbonates at Eski Gumushane section are pervasively dolomitized by fabric-destructive and fabric-preserving replacive dolomites (RD). These dolomites are Ca-rich and non-stoichiometric (Ca56-58Mg42-44). They have highly variable but low delta O-18 (-11.38 to -4.05 parts per thousand V-PDB) and delta C-13 (0.69 to 3.13 parts per thousand V-PDB) values, radiogenic Sr-87/Sr-86 ratios (0.70753 to 0.70884), extremely high Fe (2727-21053 ppm) and Mn (1548-27726 ppm) contents. Micro-crystalline quartz cement, dolomite cement and the scattered euhedral pyrite minerals (average 5 mu m) are also observed in the dissolution porosity of replacive dolomites. This study demonstrates that these carbonates have undergone a complex diagenetic history from shallow to deep burial associated with syn-sedimentary extensional tectonic activity during the Albian-Aptian and later with the hydrothermal emplacement of the polymetallic mineralization during the Eocene.", 
    "doi": "10.1007/978-3-030-01452-0_42", 
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    "meeting": {
      "title": "PALEOBIODIVERSITY AND TECTONO-SEDIMENTARY RECORDS IN THE MEDITERRANEAN TETHYS AND RELATED EASTERN AREAS"
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    "publication_date": "2019-01-01", 
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    "title": "Diagenetic Evolution of Upper Jurassic-Lower Cretaceous Berdiga Formation, NE Turkey: Petrographic and Geochemical Evidence"
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