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Lacustrine mineral facies and implications for estimation of palaeoenvironmental parameters: Neogene intervolcanic Pelitçik Basin (Galatean Volcanic Province), Turkey

Published online by Cambridge University Press:  09 July 2018

M. L. Süzen  and
A. G. Türkmenoğlu
M. L. Süzen*
Affiliation:
Department of Geological Engineering, Middle East Technical University, 06531, AnkaraTurkey
A. G. Türkmenoğlu
Affiliation:
Department of Geological Engineering, Middle East Technical University, 06531, AnkaraTurkey
*
*E-mail: [email protected]
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Abstract

The mineralogy of the Neogene lacustrine facies of Pelitçik basin was investigated for the purpose of deriving the palaeoenvironmental parameters of this intervolcanic basin. The laboratory studies indicate that dolomite and K-feldspar are the major non-clay minerals in the study area, where plagioclase, analcime, fibrous zeolite and quartz are the minor constituents. Dolomites are found to be non-stoichiometric in chemistry. The clay fraction of the lacustrine facies is composed mainly of dioctahedral smectites. The smectites are rich in Al-Fe indicating a detrital origin. Illite comprises a minor contribution to the clay fraction, where chlorite and kaolinite are found in trace amounts. Based on dolomite stoichiometry and the mineral paragenesis found in the Pelitçik basin, the depositional conditions are suggested to have been a shallow, quiet, perennial lacustrine environment with fresh to slightly saline and slightly alkaline water chemistry. In addition, based on geological and mineralogical constraints, it is suggested that the water chemistry fluctuated during the deposition of the Pazar formation and the lake began its evolution with a hydrologically closed system and completed its evolution with a hydrologically open system.

Keywords

lacustrinemineral faciesPelitçik BasinTurkeypalaeoenvironment
Type
Research Article
Information
Clay Minerals , Volume 35 , Issue 3 , June 2000 , pp. 461 - 475
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2000

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