Quick
Search: 		  
advanced search
 GSW Home   GeoRef Home   My GSW Alerts   Contact GSW   About GSW   Journals List   Help 
Clays and Clay Minerals Signup for GSW Email News
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Clays and Clay Minerals; June 2001; v. 49; no. 3; p. 197-203
© 2001 Clay Minerals Society
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Web of Science (1)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Sakharov, B. A.
Right arrow Articles by Kapron, G.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

UNUSUAL X-RAY CHARACTERISTICS OF VERMICULITE FROM WIRY, LOWER SILESIA, POLAND

Boris A. Sakharov1, Elzbieta Dubinska2, Pawel Bylina3 and Grzegorz Kapron2

1 Geological Institute, Russian Academy of Sciences, Pyzhevsky Street 7, 109017 Moscow, Russia
2 Institute of Geochemistry, Mineralogy and Petrology, Faculty of Geology, Warsaw University, al. Zwirki i Wigury 93, 02–089 Warsaw, Poland
3 Institute of Geological Sciences, Polish Academy of Sciences, ul. Twarda 51/55, 00–818 Warsaw, Poland

E-mail of corresponding author: dubinska{at}geo.uw.edu.pl

Coarse-grained vermiculite from a serpentinite-pegmatite thermal zone displays a rational series of narrow 14.4 Å basal reflections and an unusual broad 28 Å peak. X-ray diffraction simulations and fitting techniques show that the 28 Å peak is related to 28 Å domains consisting of elongated 2:1 layers of different lengths. The domains are located at the crystal edges of the vermiculite.

Key Words: Crystal Edge • Interstratified Mineral • Vermiculite • XRD Characteristics




This article has been cited by other articles:


Home page
 Clays and Clay MineralsHome page
B. A. Sakharov, B. A. Sakharov, E. Dubinska, P. Bylina, J. A. Kozubowski, G. Kapron, and M. Frontczak-Baniewicz
SERPENTINE-SMECTITE INTERSTRATIFIED MINERALS FROM LOWER SILESIA (SW POLAND)
Clays and Clay Minerals, February 1, 2004; 52(1): 55 - 65.
[Abstract] [Full Text] [PDF]


JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Clay Minerals Society