Tekke ( Amasya ) civarının jeolojisi ve tektoniği
Başlık çevirisi mevcut değil.
- Tez No: 33907
- Danışmanlar: PROF. DR. CAVİT DEMİRKOL
- Tez Türü: Yüksek Lisans
- Konular: Jeoloji Mühendisliği, Geological Engineering
- Anahtar Kelimeler: Belirtilmemiş.
- Yıl: 1994
- Dil: Türkçe
- Üniversite: Çukurova Üniversitesi
- Enstitü: Fen Bilimleri Enstitüsü
- Ana Bilim Dalı: Jeoloji Mühendisliği Ana Bilim Dalı
- Bilim Dalı: Belirtilmemiş.
- Sayfa Sayısı: 77
Özet
The Tersakan formation which crops out in the north of the study area, starts with medium-thick bedded yellowish coloured conglomerates and passes up wards into sandstones with volcanic intercalations then continue with shale - sandstone alternations. This unit deposited in the neritic and bathial environments and somehow reflecting very active (stormy) marine conditions. The volcanism also effected this condi t i ons. Upper Maestricht i an -Pal eocene aged Çatalçeş-me formation crops out in the southern and western parts of the study area and have very wide outcrops. This unit starts with yellowish-gray colured, thin medium bedded sand carbonates, shallow marine Catalcesme formation has been covered with Çekerek formation with an angular unconformity. Çekerek formation is seen in the southern part of the study area and has not a very wide outcrops in the study ares. This unit generally consists of conglomerates, sandstones, shales, sandy carbonates and aglomerates at the top. Pliocene Çerkeş- formation consists of conglomerate- sandstone alternations and presents regular bedding patterns. Lithological evidences indicate that the base of this unit is chatacterized by lacustrine environment deposits. Due to filling of this environment the deposital conditions becomes. Shallower and finally fills with continental sediments. Quaternery alluvium and alluvium cones are seen along and around the Yeşilırmak River. ftl 1 uviumdeposit s mainly consists of conglomerates, sands, clays and muds. Also, allivium cones consists of gravels, sands and clays.£.' f The Tersakan formation which crops out in the nörth of the study area, start s with medium-thick bedded yellowish colouvned conglomerat es and passes up wards into sandstones with volcanic int ercal at i ons then continue with sh^le - sandstone alternati ons. This ur» i t deposited in the neritic and bathial environment s and somehow reflecting very active (stortny) marine conditions. The volcanism also effected this condit i ons. Upper Maestricht i an-P'al eocene aged Çatalçeşme forraation crops out in the southern and western parts of the study area and have very wide outcrops. This unit start s with yellowish-gray colured, thin medium bedded sand carbonates, shallow marine Catalcesme formation has been covered with Çekerek formation with an angular unconformity. Çekerek formation i E seen in the southern part of the study area and has not a very wide outcrops in the study area This unit generally consists of conglomerates, sandstones, shales, sandy carbonates and aglomerates at the top. Pliocene Çerkeş formation consists of conglomerate- sandstone alternations and presents regular bedding patterns. Lithological evidences indicate that the base of this unit is chatacterized by lacustrine environment deposits. Due to filling of this environment the deposital conditions beccmes. Shallower and finally fills with continental sediments. Ouaternery alluvium and alluvium cones are seen along and around the Yeş-ilırmak River. fil l uviumdeposit s mainly consists of conglomerates, sands, clays and muds. ftlso, allivium cones consists of gravels, sands and clays.
Özet (Çeviri)
The Tersakan formation which crops out in the north of the study area, starts with medium-thick bedded yellowish coloured conglomerates and passes up wards into sandstones with volcanic intercalations then continue with shale - sandstone alternations. This unit deposited in the neritic and bathial environments and somehow reflecting very active (stormy) marine conditions. The volcanism also effected this condi t i ons. Upper Maestricht i an -Pal eocene aged Çatalçeş-me formation crops out in the southern and western parts of the study area and have very wide outcrops. This unit starts with yellowish-gray colured, thin medium bedded sand carbonates, shallow marine Catalcesme formation has been covered with Çekerek formation with an angular unconformity. Çekerek formation is seen in the southern part of the study area and has not a very wide outcrops in the study ares. This unit generally consists of conglomerates, sandstones, shales, sandy carbonates and aglomerates at the top. Pliocene Çerkeş- formation consists of conglomerate- sandstone alternations and presents regular bedding patterns. Lithological evidences indicate that the base of this unit is chatacterized by lacustrine environment deposits. Due to filling of this environment the deposital conditions becomes. Shallower and finally fills with continental sediments. Quaternery alluvium and alluvium cones are seen along and around the Yeşilırmak River. ftl 1 uviumdeposit s mainly consists of conglomerates, sands, clays and muds. Also, allivium cones consists of gravels, sands and clays.£.' f The Tersakan formation which crops out in the nörth of the study area, start s with medium-thick bedded yellowish colouvned conglomerat es and passes up wards into sandstones with volcanic int ercal at i ons then continue with sh^le - sandstone alternati ons. This ur» i t deposited in the neritic and bathial environment s and somehow reflecting very active (stortny) marine conditions. The volcanism also effected this condit i ons. Upper Maestricht i an-P'al eocene aged Çatalçeşme forraation crops out in the southern and western parts of the study area and have very wide outcrops. This unit start s with yellowish-gray colured, thin medium bedded sand carbonates, shallow marine Catalcesme formation has been covered with Çekerek formation with an angular unconformity. Çekerek formation i E seen in the southern part of the study area and has not a very wide outcrops in the study area This unit generally consists of conglomerates, sandstones, shales, sandy carbonates and aglomerates at the top. Pliocene Çerkeş formation consists of conglomerate- sandstone alternations and presents regular bedding patterns. Lithological evidences indicate that the base of this unit is chatacterized by lacustrine environment deposits. Due to filling of this environment the deposital conditions beccmes. Shallower and finally fills with continental sediments. Ouaternery alluvium and alluvium cones are seen along and around the Yeş-ilırmak River. fil l uviumdeposit s mainly consists of conglomerates, sands, clays and muds. ftlso, allivium cones consists of gravels, sands and clays.
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