Araştırma Makalesi
BibTex RIS Kaynak Göster

Sedımentary features of tıdal deposıts of the upper cretaceous ın seben area (NE Bolu-Turkey)

Yıl 1984, Cilt: 101-102 Sayı: 101-102, 1 - 1, 01.06.1984

Öz

Shallow water sandstones are characterized by sand bars, tidal channel and lagoon sediments, which are approximately 400 m thick of Upper Cretaceous in Seben (Bolu) area. Massive bedding, very intensive flow-rolls, parallel and low-angle cross laminations show bar sediments to be deposited near-offshore environments with high available sediments. Tidal channel had dissected upper part of bar sediments interfingering into lagoon deposits. Large-scale tabular cross bedding, various size through-cross and flame laminations, common mud nodules, lag sediments, coquina lenses, biogen burrowing zone and rippled sand surfaces, such as certain sedimentary structures suggest that the channel had been cut and filled by tidal current regimes.

Kaynakça

  • Altınlı, LE, 1973, Om Sakarya jeolojisi: Cumhuriyetin 50. Yılı Yerbilimleri Kong. Tebliğleri, 159-191, Ankara.
  • , 1975, Paleosen yaşlı Kızılçay grubunun çökelme ortamları: İst. Univ. Fen. Fak. Mecm, seri B, 40/1-2, 233-240, İstanbul.
  • Johnson, K.G. ve Friedman, G.M, 1969, The Tully clastic correlatives (Up. Devonian) of New York State; A model for recognition of alluvial, dune, tidal, nearshore (bar and lagoon) and offshore Sedimentary environments in a tectonic delta complcx: Jour. Sedim. Petrology, 39, 451-485.
  • Kazancı, N.; Varol, B. ve Tunç, M, 1984, Seben (Bolu) bölgesi Üst Kretase karbonat ve volkanojenik fliş fasiyesleri: Jeoloji Mühendisliği Derg, 20, 61-76.
  • Ludwick, J.C., 1970, Sand waves and tidal channels in the entrance to Chesapcakc Bay; Virginia: J. Science, 21, 178-184.
  • Reineck, H.E. ve Singh, I.B, 1975, Depositional Sedimentary environments: Springer Verlag, New York-Berlin- Heidelberg, 439s.
  • Saner, S, 1978, Orta Sakarya'daki Kretase-Paleosen-Eosen çökelme ilişkileri ve Anadolu'daki petrol aramalarında önemi: Türkiye 4. Petrol Kong. Bildirileri, 95-114, Ankara.
  • Sorauf, I.E, 1965, FIow rolls of Upper Devonian rocks of South Central New York State: Jour. Sedim. Petrology, 35, 553-563.
  • Swift, O.J.P, 1975, Tidal sand ridges and shoal-reueat massifs: Mar. Geol, 18, 105-134.
Yıl 1984, Cilt: 101-102 Sayı: 101-102, 1 - 1, 01.06.1984

Öz

Kaynakça

  • Altınlı, LE, 1973, Om Sakarya jeolojisi: Cumhuriyetin 50. Yılı Yerbilimleri Kong. Tebliğleri, 159-191, Ankara.
  • , 1975, Paleosen yaşlı Kızılçay grubunun çökelme ortamları: İst. Univ. Fen. Fak. Mecm, seri B, 40/1-2, 233-240, İstanbul.
  • Johnson, K.G. ve Friedman, G.M, 1969, The Tully clastic correlatives (Up. Devonian) of New York State; A model for recognition of alluvial, dune, tidal, nearshore (bar and lagoon) and offshore Sedimentary environments in a tectonic delta complcx: Jour. Sedim. Petrology, 39, 451-485.
  • Kazancı, N.; Varol, B. ve Tunç, M, 1984, Seben (Bolu) bölgesi Üst Kretase karbonat ve volkanojenik fliş fasiyesleri: Jeoloji Mühendisliği Derg, 20, 61-76.
  • Ludwick, J.C., 1970, Sand waves and tidal channels in the entrance to Chesapcakc Bay; Virginia: J. Science, 21, 178-184.
  • Reineck, H.E. ve Singh, I.B, 1975, Depositional Sedimentary environments: Springer Verlag, New York-Berlin- Heidelberg, 439s.
  • Saner, S, 1978, Orta Sakarya'daki Kretase-Paleosen-Eosen çökelme ilişkileri ve Anadolu'daki petrol aramalarında önemi: Türkiye 4. Petrol Kong. Bildirileri, 95-114, Ankara.
  • Sorauf, I.E, 1965, FIow rolls of Upper Devonian rocks of South Central New York State: Jour. Sedim. Petrology, 35, 553-563.
  • Swift, O.J.P, 1975, Tidal sand ridges and shoal-reueat massifs: Mar. Geol, 18, 105-134.
Toplam 9 adet kaynakça vardır.

Ayrıntılar

Birincil Dil İngilizce
Konular Mühendislik
Bölüm Makaleler
Yazarlar

Baki Varol Bu kişi benim

Nizamettin Kazancı

Yayımlanma Tarihi 1 Haziran 1984
Yayımlandığı Sayı Yıl 1984 Cilt: 101-102 Sayı: 101-102

Kaynak Göster

APA Varol, B., & Kazancı, N. (1984). Sedımentary features of tıdal deposıts of the upper cretaceous ın seben area (NE Bolu-Turkey). Bulletin of the Mineral Research and Exploration, 101-102(101-102), 1-1.
AMA Varol B, Kazancı N. Sedımentary features of tıdal deposıts of the upper cretaceous ın seben area (NE Bolu-Turkey). Bull.Min.Res.Exp. Haziran 1984;101-102(101-102):1-1.
Chicago Varol, Baki, ve Nizamettin Kazancı. “Sedımentary Features of tıdal deposıts of the Upper Cretaceous ın Seben Area (NE Bolu-Turkey)”. Bulletin of the Mineral Research and Exploration 101-102, sy. 101-102 (Haziran 1984): 1-1.
EndNote Varol B, Kazancı N (01 Haziran 1984) Sedımentary features of tıdal deposıts of the upper cretaceous ın seben area (NE Bolu-Turkey). Bulletin of the Mineral Research and Exploration 101-102 101-102 1–1.
IEEE B. Varol ve N. Kazancı, “Sedımentary features of tıdal deposıts of the upper cretaceous ın seben area (NE Bolu-Turkey)”, Bull.Min.Res.Exp., c. 101-102, sy. 101-102, ss. 1–1, 1984.
ISNAD Varol, Baki - Kazancı, Nizamettin. “Sedımentary Features of tıdal deposıts of the Upper Cretaceous ın Seben Area (NE Bolu-Turkey)”. Bulletin of the Mineral Research and Exploration 101-102/101-102 (Haziran 1984), 1-1.
JAMA Varol B, Kazancı N. Sedımentary features of tıdal deposıts of the upper cretaceous ın seben area (NE Bolu-Turkey). Bull.Min.Res.Exp. 1984;101-102:1–1.
MLA Varol, Baki ve Nizamettin Kazancı. “Sedımentary Features of tıdal deposıts of the Upper Cretaceous ın Seben Area (NE Bolu-Turkey)”. Bulletin of the Mineral Research and Exploration, c. 101-102, sy. 101-102, 1984, ss. 1-1.
Vancouver Varol B, Kazancı N. Sedımentary features of tıdal deposıts of the upper cretaceous ın seben area (NE Bolu-Turkey). Bull.Min.Res.Exp. 1984;101-102(101-102):1-.

Copyright and Licence
The Bulletin of Mineral Research and Exploration keeps the Law on Intellectual and Artistic Works No: 5846. The Bulletin of Mineral Research and Exploration publishes the articles under the terms of “Creatice Common Attribution-NonCommercial-NoDerivs (CC-BY-NC-ND 4.0)” licence which allows to others to download your works and share them with others as long as they credit you, but they can’t change them in any way or use them commercially.

For further details;
https://creativecommons.org/licenses/?lang=en