Search Results - "Levent Karadenizli"

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  1. 1

    Oligocene to Pliocene palaeogeographic evolution of the Çankırı-Çorum Basin, central Anatolia, Turkey by Karadenizli, Levent

    Published in Sedimentary geology (15-05-2011)
    “…The Çankırı-Çorum Basin is one of the largest basins of Central Anatolia to have developed Oligocene to Quaternary terrestrial environments. The basin contains…”
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    Journal Article
  2. 2

    Oligocene to Pliocene palaeogeographic evolution of the Çankr-Çorum Basin, central Anatolia, Turkey by Karadenizli, Levent

    Published in Sedimentary geology (15-05-2011)
    “…The Çankr-Çorum Basin is one of the largest basins of Central Anatolia to have developed Oligocene to Quaternary terrestrial environments. The basin contains…”
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    Journal Article
  3. 3

    Sea-level changes and related depositional environments on the southern Marmara shelf by Ergin, Mustafa, Kazanci, Nizamettin, Varol, Baki, Ileri, Özden, Levent Karadenizli

    Published in Marine geology (01-08-1997)
    “…Petrographic data obtained from 182 surface sediment samples together with the available bathymetric data are used to investigate the effects of the last major…”
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  4. 4

    Palaeoclimatic and palaeoenvironmental interpretations of the Late Oligocene, Late Miocene–Early Pliocene in the Çankırı-Çorum Basin by Kayseri-Özer, Mine Sezgül, Karadenizli, Levent, Akgün, Funda, Oyal, Neşe, Saraç, Gerçek, Şen, Şevket, Tunoğlu, Cemal, Tuncer, Alaettin

    “…Palaeoclimatic and palaeoenvironmental interpretations are reconstructed from the sedimentary sequences of the Late Oligocene and Miocene–Pliocene boundary in…”
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  5. 5

    Late Eocene-early Miocene palaeogeographic evolution of central eastern Anatolian basins, the closure of the Neo-Tethys ocean and continental collision by Karadenizli, Levent, Varol, Baki Erdogan, Saraç, Gerçek, Gedik, Fatma

    Published in Journal of the Geological Society of India (01-12-2016)
    “…In central eastern Anatolia which is located between Eurasia and Africa, the study of basin developments between late Eocene and early Miocene is of great…”
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    A giant rhinocerotoid (Mammalia, Perissodactyla) from the Late Oligocene of north-central Anatolia (Turkey) by ANTOINE, PIERRE-OLIVIER, KARADENIZLI, LEVENT, SARAÇ, GERÇEK, SEN, SEVKET

    Published in Zoological journal of the Linnean Society (01-03-2008)
    “…A giant rhinocerotoid is described for the first time south of the Black Sea, in Turkey. The single specimen, a fragmentary radius referred to Paraceratherium…”
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    Lithostatigraphy and mammalian fossil content of lower miocene deposits in the westeren part of the Çankırı basin; A test for post-collisional tectonic models of NW central Anatolia by ÖZCAN, Fatih, KARADENİZLİ, Levent, SARAÇ, Gerçek, ŞEN, Şevket, SEYİTOĞLU, Gürol

    Published in Türkiye jeoloji bülteni (2007)
    “…Çankırı havzasının batı kenarında yapılan ayrıntılı jeolojik harita alımı, Neojen birimlerin tabanını oluşturan Kılçak formasyonunun bir tektonik kamanın her…”
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  11. 11

    ÇANKIRI-ÇORUM HAVZASI BATI KENARININ ERKEN-ORTA MİYOSEN PALEOCOĞRAFİK EVRİMİ by Levent KARADENİZLİ, Gürol SEYİTOĞLU, Gerçek SARAÇ, Nizamettin KAZANCI, Şevket ŞEN, Yavuz HAKYEMEZ, Didem SAVAŞÇI

    “…Çankırı-Çorum havzası, Orta Anadolu'da Tersiyer'de gelişen havzalardan birisidir ve Paleosen'den Pliyosen'e kadar önemli tortul birikimine sahip olmuştur. Bu…”
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  12. 12

    Beypazarı havzası (Ankara batısı) üst miyosen-pliyosen jipsli serilerinin sedimantolojisi by KARADENİZLİ, Levent

    Published in Türkiye jeoloji bülteni (1995)
    “…Üst Miyosen-PIiyosen yaşlı Kirmir formasyonunun temel litolojisini jips ve kiltaşları oluşturur. Bu birim tabanda Üst Miyosen yaşlı Bozbelen formasyonu…”
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  13. 13

    Çankırı-Çorum havzası batı kenarının Erken-Orta Miyosen paleocoğrafik evrimi by SAVAŞCI, Didem, KARADENİZLİ, Levent, KAZANCI, Nizamettin, HAKYEMEZ, Yavuz, SARAÇ, Gerçek, SEYİTOĞLU, Gürol, ŞEN, Şevket

    Published in Maden Tetkik ve Arama Dergisi (2003)
    “…Çankırı-Çorum havzası, Orta Anadolu'da Tersiyer'de gelişen havzalardan birisidir ve Paleosen'den Pliyosen'e kadar önemli tortul birikimine sahip olmuştur. Bu…”
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    Journal Article