- 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 Key Takeaways
🎯
Objective & Hypothesis:- 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
📊
Key Findings & Data:- 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
💡
Conclusion & Impact:- 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
🔬Design:Research Article
📍Scope:Comprehensive Sample
⚙️Variables:Domain Parameters
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
🔖
Cite This Article
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/54285
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.
Fairbridge, R.W., 1968, Atlantic and Pasific Type Coasts: Fairbridge, R.W., ed., Encyclopedia of Earth Sciences Series Vol. lll'de. Reinhold Book Corp., New York, 34-35.
Gadow, S. ve Reineck. H.E., 1968, Der Abbau amer magnetit-strandseife in Italien: Natur. Mus., 98, 57-63.
Hakyemez, H.Y. ve Erkal, T., 1994, Trakya'nın Karadeniz Kıyı Kuşağındaki Plaser Rutilin Örneklemesi, Kaynak Alanı ve Dağılımına ilişkin Sedimentolojik ve Jeomorfolojik Etüt Raporu: MTA Rap., 9678 (yayımlanmamış) 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.
Yurtsever, A.; Arda, A. ve Özcan, l., 1994, Yıldı z Dağları (Istranca Masifi'nin Jeolojisi: MTA Rap. (basımda) Ankara.