Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Mineralogical Magazine Don't get GSW? Talk to your librarian.
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Mineralogical Magazine; December 2000; v. 64; no. 6; p. 1007-1016
© 2000 Mineralogical Society of Great Britain and Ireland
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
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
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 Google Scholar
Google Scholar
Right arrow Articles by Graupner, T.
Right arrow Articles by Wolf, D.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

CL for characterizing quartz and trapped fluid inclusions in mesothermal quartz veins: Muruntau Au ore deposit, Uzbekistan

T. Graupner*, J. Götze, U. Kempe and D. Wolf

Institute of Mineralogy, Freiberg University of Mining and Technology, Brennhausgasse 14, D-09596 Freiberg, Germany

* E-mail: graupner{at}mineral.tu-freiberg.de

Combined cathodoluminescence (CL) and transmitted light microscopy were used to characterize quartz from flat and steeply dipping quartz veins and from veinlets in banded host rocks from the giant Muruntau Au quartz vein deposit, Kyzyl Kum Desert, western Uzbekistan. The CL examinations were carried out using a ‘hot-cathode’ CL microscope linked to a highly sensitive digital video camera. The multi-stage deformed flat quartz veins and the steeply dipping hydrothermal formations at Muruntau are characterized by quartz with different CL colours, internal structures and degree of secondary alteration. Primary growth zoning of quartz, indiscernible in conventional polarized light was found to occur only in steeply dipping veins. The bulk of the high-grade Au mineralized ‘central’ quartz veins is dominated by one generation of hydrothermal quartz; intense brecciation of these veins is indicated by the occurrence of fragments of zoned quartz crystals. Primary growth zoning in quartz may be revealed not only by variations in the intensity of blue CL and/or by primary fluid inclusions arranged within the zones, but also by secondary inclusions and recrystallization phenomena developed along boundary surfaces between the zones. Using the results from CL imaging and microstructural analysis of the quartz, fluid inclusions investigated earlier were assigned to genetic types; the evidence of probably primary inclusions is of considerable importance for further studies of the geochemical conditions during vein formation. Considering geological and mineralogical data, CL studies of vein quartz may help to reveal the history of precipitation, deformation and recrystallization processes in the Muruntau Au ore field.

KEYWORDS: cathodoluminescence, quartz, fluid inclusions, Au ore deposit, Muruntau, Uzbekistan




This article has been cited by other articles:


Home page
American MineralogistHome page
B. G. Rusk, M. H. Reed, J. H. Dilles, and A. J.R. Kent
Intensity of quartz cathodoluminescence and trace-element content in quartz from the porphyry copper deposit at Butte, Montana
American Mineralogist, August 1, 2006; 91(8-9): 1300 - 1312.
[Abstract] [Full Text] [PDF]


Home page
Geological Society, London, Special PublicationsHome page
S. Michalski, J. Gotze, H. Siedel, M. Magnus, and R. B. Heimann
Investigations into provenance and properties of ancient building sandstones of the Zittau/Gorlitz region (Upper Lusatia, Eastern Saxony, Germany)
Geological Society, London, Special Publications, January 1, 2002; 205(1): 283 - 297.
[Abstract] [PDF]


Home page
Economic GeologyHome page
T. Graupner, T. GRAUPNER, U. KEMPE, E. T.C. SPOONER, C. J. BRAY, A. A. KREMENETSKY, and G. IRMER
Microthermometric, Laser Raman Spectroscopic, and Volatile-Ion Chromatographic Analysis of Hydrothermal Fluids in the Paleozoic Muruntau Au-Bearing Quartz Vein Ore Field, Uzbekistan
Economic Geology, January 1, 2001; 96(1): 1 - 23.
[Abstract] [Full Text] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2008 by Mineralogical Society of Great Britain and Ireland