Basement types, Eocene Series, Upper Eocene Olistostromes and the Initiation of Southern Thrace Basin, NW Turkey
Turkish Journal of Earth Science, No. 19, Ocak 2009, s. 1-24
OKAY AI, OZCAN E, CAVAZZA W, OKAY N, LESS G
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Provenance of turbidite sands in the Marmara Sea, Turkey: A tool for submarine paleoseismology
GSA, 8 Ekim 2004
GEORGE LOZEFSKİ,MCHUGH CECİLİA,CORMİER MİLENE,SEEBER LEONARDO,ÇAĞATAY MEMET NAMIK,OKAY NİLGÜN
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Source of the Carboniferous Flysch of the İstanbul Zone: Sandstone Petrography and Detrital Zircon-Rutile Geochronology
18th International Petroleum and Natural Gas Congress and Exhibition of Turkey, 11 Mayıs 2011
OKAY NİLGÜN,ZACK THOMAS,OKAY ARAL
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Detrital rutile ages from the Carboniferous flysch of the Istanbul Zone, Turkey: New Insights for Provenance Studies
GSA Tectonic Crossroads: Evolving Orogens of Eurasia-Africa-Arabia Symposium, Geological Society of America, Ankara/TÜRKİYE, 4 Ekim 2010, s. 67
ZACK THOMAS,OKAY NİLGÜN,OKAY ARAL
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An Olistostrome melange belt formed along a major strike slip tear fault Bornova Flysh Zone Western Turkey
Tectonophysics, Vol. 2, No. 10, 2012, s. 1-20
OKAY ARAL,IŞINTEK İSMAİL,ALTİNER DEMİR,OZKAN ALTİNER SEVİNÇ,OKAY NİLGÜN
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An active, deep marine strike-slip basin along the North Anatolian Fault in Turkey
Tectonics, No. 18, Nisan 1999, s. 129-148
OKAY A I, DEMIRBAG E, KURT H, OKAY N, KUSCU I
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Basement types, Eocene Series, Upper Eocene Olistostromes and the Initiation of Southern Thrace Basin, NW Turkey
Turkish Journal of Earth Science, No. 19, Ocak 2010, s. 1-24
OKAY AI, OZCAN E, CAVAZZA W, OKAY N, LESS G
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Active faults and strike-slip basins in the Marmara Sea, northwest Turkey
International Earth Sciences Colloquium on the Aegean Region, IEASCA-2, Eylül 2000, s. 6
OKAY A.I. ET AL.
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Detrital rutile ages from the Carboniferous flysch of the Istanbul Zone, Turkey: new insights for provenance studies.
Tectonic Crossroads: Evolving Orogens of Eurasia-Africa-Arabia, Geolog, Ekim 2010, s. 67
ZACK T., OKAY N., OKAY A.I.
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Bornova Fliş Zonu: Litosferik Ölçekte Yanal-Atımlı Bir Yırtılma Fayı Boyunca Oluşan Olistostrom-Melanj Kuşağı.
64. Geological Congress of Turkey, Nisan 2011, s. 26-27
OKAY A.I ET AL.
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Was the Maritsa river flowing into the Marmara basin during the Early Quaternary?
Workshop on the Quaternary in Turkey, Mayıs 2001, s. 52-53
, OKAY A.I., OKAY N.
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The Tectonic Setting of the Ophiolitic Mélange and the Intra-Pontide Suture in the Southern Thrace and the Initiation of the Thrace Basin.
62. Geological Congress of Turkey, Nisan 2009, s. 452-453
OKAY A.I., TOPUZ G., OZCAN E., CAVAZZA W., OKAY N.
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The Tectonic Setting of the Ophiolitic Mélange and the Intra-Pontide Suture in the Southern Thrace and the Initiation of the Thrace Basin.
62. Geological Congress of Turkey, Nisan 2009, s. 452-453
, OKAY A.I., TOPUZ G., OZCAN E., CAVAZZA W., OKAY N.
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The formation of the Tekirdağ basin in the Marmara Sea
Marine Geological and Geophysical Research in Turkey, Workshop-IV, Eylül 1998, s. 1-3
OKAY A.I., DEMIRBAG E., KURT H., OKAY N., KUSCU I.
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Was the Maritsa river flowing into the Marmara basin during the Early Quaternary?
Workshop on the Quaternary in Turkey, Mayıs 2001, s. 52-53
OKAY A.I., OKAY N.
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Current Status of women in Geosciences: A case study from Turkey.
32. Interntional Geological Congress, Ağustos 2004
OKAY N., GUNEY A., ARSLAN F., UNAL Y.
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A Guide for developing emergency plan for museums in Turkey
ICOMOS International Symposium Cultural Hertage Protection in Times of, Kasım 2012
SUNGUR B., KADIOGLU M., OKAY N.
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A Guide for developing emergency plan for museums in Turkey
ICOMOS International Symposium Cultural Hertage Protection in Times of, Kasım 2012
SUNGUR B., KADIOGLU M., OKAY N.
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Provenance of turbidite sands in the Marmara Sea, Turkey: A tool for submarine paleoseismology
Northestern Section (39th Annual) and Southeastern Section (53rd Annua, Mart 2004
LOZEFSKI G., MCHUGH C., CORMIER M-H., SEEBER L. ET AL., R/V URANIA 2000 TEAM
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An Olistostrome-melange belt formed along a major strike-slip tear fault: Bornova Flysh Zone, Western Turkey
Tectonophysics, Ocak 2013
OKAY A, ISINTEK I, ALTINER D, ALTINER S, OKAY N
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