Jeoloji Münendisliği Dergisi
Jeoloji Mühendisliği Dergisi

Jeoloji Mühendisliği Dergisi

1978 ŞUBAT Cilt 2 Sayı 1
COVER
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COPYRİHT PAGE
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CONTENTS
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TO OUR READERS
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ARTİCLE
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Hasan Özaslan
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  • Aslan, Ö . (1978). YEŞİLDERE HEYELANI . Jeoloji Mühendisliği Dergisi , 2 (1) , 7-8 . Retrieved from https://dergipark.org.tr/tr/pub/jmd/issue/28149/296159

  • Aslan, Ö . YEŞİLDERE HEYELANI. Jeoloji Mühendisliği Dergisi 2 (1978 ): 7-8

  • Egon T. Degens Francis Khoo Walter Miohaelis Boğan Aksoy Güles Bor
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    ABSTBACT: The upper 90 cm of Black Sea basin sediment with an aereal extension of 2,96X105 km2 has an U8O8 content of 6.7X106 tonnes, Plankton is the prime agent for uranium to accumulate over the past 5,000 yr. Energetically self-sufficient burning of the top 1-m strata will lead to U8O8 concentrations in the order öf 100 g per tonne ash.



  • Degens, E , Khoo, F , Michales, W . (1978). Karadeniz Sedimanlarındaki Uranyum Anomalisi . Jeoloji Mühendisliği Dergisi , 2 (1) , 9-13 . Retrieved from https://dergipark.org.tr/tr/pub/jmd/issue/28149/296162

  • Degens, E , Khoo, F , Michales, W . Karadeniz Sedimanlarındaki Uranyum Anomalisi. Jeoloji Mühendisliği Dergisi 2 (1978 ): 9-13

  • Gürkan Yersel
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  • Yersel, G . (1978). KARBONATİT MADEN YATAKLARI . Jeoloji Mühendisliği Dergisi , 2 (1) , 14-17 . Retrieved from https://dergipark.org.tr/tr/pub/jmd/issue/28149/296165

  • Yersel, G . KARBONATİT MADEN YATAKLARI. Jeoloji Mühendisliği Dergisi 2 (1978 ): 14-17

  • Talip Karaoğullarindan
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  • Karagül, T . (1978). Toprak Barajlarda Filişlerden Geçirimsiz Çekirdek Malzemesi Yapımı . Jeoloji Mühendisliği Dergisi , 2 (1) , 18-26 . Retrieved from https://dergipark.org.tr/tr/pub/jmd/issue/28149/296170

  • Karagül, T . Toprak Barajlarda Filişlerden Geçirimsiz Çekirdek Malzemesi Yapımı. Jeoloji Mühendisliği Dergisi 2 (1978 ): 18-26

  • İsmail Seyhan
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    ABSTRACT:  Many of the Turkish kaolin deposits are hydrothermal type although some of the country`s major deposits are believed to have originated from weathering. Intensive silicification and limonitization and the associated hydrothermal ores such as mercury, antimony, fluorite and sulfur minerals are taken as indication to hydrothermal origin. The thickness of the hydrothermal kaolin deposits controlled by volcanic phenomena is, generally speaking, comparatively less, where as their lateral persistances often considerable* Those oecuring within the fault zones, however, attain considerable thickness — locally as much as 100 meters. Bulk of the Turkish kaolin deposits formed by hydrothermal actions are presently considered uneconomic due to extensive alunitization, and the associated pyrite, and sulfur formations and 3b, Hg, Pb, Zn, Cu, Ni, and Co - sulfide minerals. Chemical processes associated with kaolinization are believed to have led to the high concentrations of metallic ores, which in turn caused considerable changes in the pH - conditions of the deposit, thus resulting in marked increases in the illite and montmorülonite content of these deposits*



  • Seyhan, İ . (1978). TÜRKİYE KAOLİN YATAKLARI İLE HİDROTERMAL CEVHERLER ARASINDA GÖRÜLEN İLİŞKİLER* . Jeoloji Mühendisliği Dergisi , 2 (1) , 27-31 . Retrieved from https://dergipark.org.tr/tr/pub/jmd/issue/28149/296171

  • Seyhan, İ . TÜRKİYE KAOLİN YATAKLARI İLE HİDROTERMAL CEVHERLER ARASINDA GÖRÜLEN İLİŞKİLER. Jeoloji Mühendisliği Dergisi 2 (1978 ): 27-31

  • J.a. Franklin Hasan Özaslan
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  • Franklin, J . (1978). Kaya Yapı Gereçlerinin Çıkarılması ve İşletilmesi İle İlgili Kaya Niteliği . Jeoloji Mühendisliği Dergisi , 2 (1) , 32-39 . Retrieved from https://dergipark.org.tr/tr/pub/jmd/issue/28149/296173

  • Franklin, J . Kaya Yapı Gereçlerinin Çıkarılması ve İşletilmesi İle İlgili Kaya Niteliği. Jeoloji Mühendisliği Dergisi 2 (1978 ): 32-39

  • Salih Gök
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  • Gök, S . (1978). TÜRKİYE NEOJEN FORMASYONLARININ EKONOMİK JEOLOJİSİ . Jeoloji Mühendisliği Dergisi , 2 (1) , 40-59 . Retrieved from https://dergipark.org.tr/tr/pub/jmd/issue/28149/296180

  • Gök, S . TÜRKİYE NEOJEN FORMASYONLARININ EKONOMİK JEOLOJİSİ. Jeoloji Mühendisliği Dergisi 2 (1978 ): 40-59

  • ISSUE FULL FİLE
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