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Clay minerals from Permo-Carboniferous very low-grade metamorphic rocks from the central part of the Fore Sudetic Monocline (western Poland)

Published online by Cambridge University Press:  09 July 2018

E. T. Sokalska ,
E. Dubińska ,
G. Kaproń ,
J. A. Kozubowski  and
M. Walski
E. T. Sokalska*
Affiliation:
Institute of Geochemistry, Mineralogy and Petrology, Faculty of Geology, Warsaw University, al. Żwirki i Wigury 93, 02-089 Warsaw, Poland
E. Dubińska
Affiliation:
Institute of Geochemistry, Mineralogy and Petrology, Faculty of Geology, Warsaw University, al. Żwirki i Wigury 93, 02-089 Warsaw, Poland
G. Kaproń
Affiliation:
Institute of Geochemistry, Mineralogy and Petrology, Faculty of Geology, Warsaw University, al. Żwirki i Wigury 93, 02-089 Warsaw, Poland
J. A. Kozubowski
Affiliation:
Faculty of Materials Science and Engineering, Warsaw University of Technology, 141 Woloska Str., 02-507 Warsaw, Poland
M. Walski
Affiliation:
Department of Cell Ultrastructure, Medical Research Centre, Polish Academy of Sciences, 5 Pawińskiego Str., 02-106 Warsaw, Poland
*
*E-mail: e.t.sokalska@uw.edu.pl
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Abstract

The mafic rocks from boreholes studied here contain the assemblage typical for upper-subgreenschist to lower-greenschist facies (albite, chlorite, illite, titanite, quartz, Ti-oxide ± actinolite) as well as relict clinopyroxene.Metapelites underlying a metabasic rock sequence also record metamorphic alteration as demonstrated by the chlorite and illite crystallinities. Chlorite crystallinity suggests formation in conditions close to the subgreenschist/greenschist facies boundary, but this mineral is partly decomposed during metamorphic retrogression.

Keywords

metabasic rocksmetapelitesXRDHRTEMchlorite crystallinitygreenschist-facies metamorphismsubgreenschist-facies metamorphismFore Sudetic Monocline
Type
Research Article
Information
Clay Minerals , Volume 43 , Issue 4 , December 2008 , pp. 561 - 574
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2008

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Footnotes

†

Deceased

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