- In order to carry out the plaser investigation on a coastal zone, it is necessary 1° to define the sedimentary sub-basins and source area of these basins, 2° to differentiate the geomorphtc units and sedimentary facies, and 3° to collect the representative samples from these facies By this way it is possible to find where the tenof increases; in which coastal sub-zone and sedimentary sub-basin fed by which source area This method has been carried out in the Thracian coastal zone of the Black Sea So it has been understood that the plaser rutile is concentrated in winter-beach and that the higher percentage of rutile defined in the coastal zone near the Ormanlı village fed by a source area mainly composed of the upper Miocene aged Ergene formation
📌 3 Maddede Bu Makale
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Amaç & Hipotez:- In order to carry out the plaser investigation on a coastal zone, it is necessary 1° to define the sedimentary sub-basins and source area of these basins, 2° to differentiate the geomorphtc units and sedimentary facies, and 3° to collect the representative samples from these facies By this way it is possible to find where the tenof increases; in which coastal sub-zone and sedimentary sub-basin fed by which source area This method has been carried out in the Thracian coastal zone of the Black Sea So it has been understood that the plaser rutile is concentrated in winter-beach and that the higher percentage of rutile defined in the coastal zone near the Ormanlı village fed by a source area mainly composed of the upper Miocene aged Ergene formation
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Temel Bulgular & Veri:- In order to carry out the plaser investigation on a coastal zone, it is necessary 1° to define the sedimentary sub-basins and source area of these basins, 2° to differentiate the geomorphtc units and sedimentary facies, and 3° to collect the representative samples from these facies By this way it is possible to find where the tenof increases; in which coastal sub-zone and sedimentary sub-basin fed by which source area This method has been carried out in the Thracian coastal zone of the Black Sea So it has been understood that the plaser rutile is concentrated in winter-beach and that the higher percentage of rutile defined in the coastal zone near the Ormanlı village fed by a source area mainly composed of the upper Miocene aged Ergene formation
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Sonuç & Katkı:- In order to carry out the plaser investigation on a coastal zone, it is necessary 1° to define the sedimentary sub-basins and source area of these basins, 2° to differentiate the geomorphtc units and sedimentary facies, and 3° to collect the representative samples from these facies By this way it is possible to find where the tenof increases; in which coastal sub-zone and sedimentary sub-basin fed by which source area This method has been carried out in the Thracian coastal zone of the Black Sea So it has been understood that the plaser rutile is concentrated in winter-beach and that the higher percentage of rutile defined in the coastal zone near the Ormanlı village fed by a source area mainly composed of the upper Miocene aged Ergene formation
🔬Tür:Araştırma Makalesi
📍Kapsam:Genişletilmiş Akademik Örneklem
⚙️Değişkenler:Alan Parametreleri
Abstract
- In order to carry out the plaser investigation on a coastal zone, it is necessary 1° to define the sedimentary sub-basins and source area of these basins, 2° to differentiate the geomorphtc units and sedimentary facies, and 3° to collect the representative samples from these facies By this way it is possible to find where the tenof increases; in which coastal sub-zone and sedimentary sub-basin fed by which source area This method has been carried out in the Thracian coastal zone of the Black Sea So it has been understood that the plaser rutile is concentrated in winter-beach and that the higher percentage of rutile defined in the coastal zone near the Ormanlı village fed by a source area mainly composed of the upper Miocene aged Ergene formation
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Bu Makaleye Atıf Yap
Hakyemez, H. Y., Erkal, T. (1994). RESEARCH METHOD ON BEACH PLASER DEPOSITS CASE STUDY FROM THE THRACIAN COASTAL ZONE OF THE BLACK SEA, TURKEY. Maden Tetkik ve Arama Dergisi, Cilt: 116 Sayı: 116, 46–46. https://ajindex.com/articles/1120254
Erol, O., 1991, Türkiye kıyılarındaki terkedilmiş tarihi limanlar: Bir çevre sorunu olarak kıyı çizgisi değişimlerinin önemi: ist. Üniv. Deniz Bilimleri ve Coğr. Enst. Bülteni, 8, 1-44.
ve Altın, B.N., 1991, Binkılıç-Karacaköy dolayının jeomorfolojisi, Istranca Dağları, Trakya (Geomorphology of the Binkılıç-Karacaköy area, Southeastern part of the Yıldız "Istranca" Mountains, Thrace, Northwest Turkey): Coğrafya Araştırmaları, 3, 1 73-188.
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Umut, M.; Kurt, Z,; imik, M.; Özcan, l.; Sarıkaya, H. ve Saraç, G. 1983, Tekirdağ Ili-Silivri (istanbul Ili)-Pınarhisar (Kırklareli ili) Alanının Jeolojisi: MTA Rap. 7349 (yayımlanmamış) Ankara.
Yurtsever, A.; Arda, A. ve Özcan, l., 1994, Yıldı z Dağları (Istranca Masifi'nin Jeolojisi: MTA Rap. (basımda) Ankara.
Umut, M.; Kurt, Z,; imik, M.; Özcan, l.; Sarıkaya, H. ve Saraç, G. 1983, Tekirdağ Ili-Silivri (istanbul Ili)-Pınarhisar (Kırklareli ili) Alanının Jeolojisi: MTA Rap. 7349 (yayımlanmamış) Ankara.