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

Year 1984, Volume: 101-102 Issue: 101-102, 1 - 1, 01.06.1984

Abstract

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.

References

  • 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.
Year 1984, Volume: 101-102 Issue: 101-102, 1 - 1, 01.06.1984

Abstract

References

  • 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.
There are 9 citations in total.

Details

Primary Language English
Subjects Engineering
Journal Section Articles
Authors

Baki Varol This is me

Nizamettin Kazancı

Publication Date June 1, 1984
Published in Issue Year 1984 Volume: 101-102 Issue: 101-102

Cite

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. June 1984;101-102(101-102):1-1.
Chicago Varol, Baki, and 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, no. 101-102 (June 1984): 1-1.
EndNote Varol B, Kazancı N (June 1, 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 and N. Kazancı, “Sedımentary features of tıdal deposıts of the upper cretaceous ın seben area (NE Bolu-Turkey)”, Bull.Min.Res.Exp., vol. 101-102, no. 101-102, pp. 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 (June 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 and Nizamettin Kazancı. “Sedımentary Features of tıdal deposıts of the Upper Cretaceous ın Seben Area (NE Bolu-Turkey)”. Bulletin of the Mineral Research and Exploration, vol. 101-102, no. 101-102, 1984, pp. 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-.

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