Turkish with English abstract

E. Bayhan; G. Ataman

Turkish with English abstract

E. Bayhan
, G. Ataman

Hacettepe University

Hacettepe University

Research output: Contribution to journal › Article › peer-review

Abstract

A study was made of measured stratigraphic sections of these flysch deposits, which lie SW, S and E of Ankara, Turkey. Petrographic descriptions and XRD data on clay fractions of samples collected from the flysch series are presented. The sandstones are mostly of greywacke and subordinate greywacke type, whereas the limestones are mostly biosparites and biomicrites. Vertical and lateral variations of clay fractions were investigated, and smectite was found to be the dominant clay mineral in the Upper Cretaceous formation, while corrensite and 14_s-14_c mixed series are dominant in the Palaeocene and Lower Eocene series. Smectite is again dominant in the Middle Eocene series. -P.Br.

Translated title of the contribution	(Sedimentological properties and clay mineralogy of Upper Cretaceous-Lower Tertiary flysch deposits in the Ankara virgation.)
Original language	English
Pages (from-to)	57-72
Number of pages	16
Journal	Yerbilimleri/ Earth Sciences
Volume	9
Publication status	Published - 1982

Cite this

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title = "Turkish with English abstract",

abstract = "A study was made of measured stratigraphic sections of these flysch deposits, which lie SW, S and E of Ankara, Turkey. Petrographic descriptions and XRD data on clay fractions of samples collected from the flysch series are presented. The sandstones are mostly of greywacke and subordinate greywacke type, whereas the limestones are mostly biosparites and biomicrites. Vertical and lateral variations of clay fractions were investigated, and smectite was found to be the dominant clay mineral in the Upper Cretaceous formation, while corrensite and 14s-14c mixed series are dominant in the Palaeocene and Lower Eocene series. Smectite is again dominant in the Middle Eocene series. -P.Br.",

author = "E. Bayhan and G. Ataman",

year = "1982",

language = "English",

volume = "9",

pages = "57--72",

journal = "Yerbilimleri/ Earth Sciences",

issn = "1301-2894",

publisher = "Hacettepe Universitesi Yerbilmleri",

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TY - JOUR

T1 - Turkish with English abstract

AU - Bayhan, E.

AU - Ataman, G.

PY - 1982

Y1 - 1982

N2 - A study was made of measured stratigraphic sections of these flysch deposits, which lie SW, S and E of Ankara, Turkey. Petrographic descriptions and XRD data on clay fractions of samples collected from the flysch series are presented. The sandstones are mostly of greywacke and subordinate greywacke type, whereas the limestones are mostly biosparites and biomicrites. Vertical and lateral variations of clay fractions were investigated, and smectite was found to be the dominant clay mineral in the Upper Cretaceous formation, while corrensite and 14s-14c mixed series are dominant in the Palaeocene and Lower Eocene series. Smectite is again dominant in the Middle Eocene series. -P.Br.

AB - A study was made of measured stratigraphic sections of these flysch deposits, which lie SW, S and E of Ankara, Turkey. Petrographic descriptions and XRD data on clay fractions of samples collected from the flysch series are presented. The sandstones are mostly of greywacke and subordinate greywacke type, whereas the limestones are mostly biosparites and biomicrites. Vertical and lateral variations of clay fractions were investigated, and smectite was found to be the dominant clay mineral in the Upper Cretaceous formation, while corrensite and 14s-14c mixed series are dominant in the Palaeocene and Lower Eocene series. Smectite is again dominant in the Middle Eocene series. -P.Br.

UR - https://www.scopus.com/pages/publications/0019937415

M3 - Article

AN - SCOPUS:0019937415

SN - 1301-2894

VL - 9

SP - 57

EP - 72

JO - Yerbilimleri/ Earth Sciences

JF - Yerbilimleri/ Earth Sciences

ER -

Turkish with English abstract

Abstract

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