Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
American Mineralogist house ad
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

American Mineralogist; July; v. 93; no. 7; p. 1034-1042; DOI: 10.2138/am.2008.2727
© 2008 Mineralogical Society of America
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 Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via Web of Science (2)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Thomas, R.
Right arrow Articles by Hahn, A.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Ramanite-(Cs) and ramanite-(Rb): New cesium and rubidium pentaborate tetrahydrate minerals identified with Raman spectroscopy

Rainer Thomas1,*, Paul Davidson2 and Andreas Hahn1

1 GeoForschungsZentrum Potsdam, Telegrafenberg B120, D-14473 Potsdam, Germany
2 ARC Centre of Excellence in Ore Deposits, University of Tasmania, Hobart 7001, Australia

Correspondence: * E-mail: thomas{at}gfz-potsdam.de

This study of melt and fluid inclusions in graphic pegmatite quartz from the Island of Elba, Italy has identified silicate melts and coexisting aqueous fluid from the final stage of pegmatite formation, which contain extremely high concentrations of boron (up to 19.8 mass% B2O3), cesium (>5 mass% Cs2O), and rubidium (>0.5 mass% Rb2O). Several boron-bearing minerals have been identified in melt and fluid inclusions, including sassolite (H3BO3) and santite (KB5O8·4H2O). In addition, we have found two new minerals observed as daughter mineral phases, and these have been accepted by the IMA, Commission on New Minerals, Nomenclature and Classification (CNMNC) as ramanite-(Cs) (2007-007), monoclinic β-cesium pentaborate tetrahydrate (CsB5O8·4H2O) with space group C2/c, and ramanite-(Rb) (2007-006), orthorhombic rubidium pentaborate tetrahydrate (RbB5O8·4H2O) with space group Aba2.

At the moment, given sample constraints, we cannot directly determine some of the properties traditionally reported for new minerals; however, both phases have Raman spectra identical to spectra obtained on synthetic Cs and Rb pentaborates, which were studied for comparison. Although difficult to recognize optically, ramanite-(Cs) and ramanite-(Rb) have distinctive Raman spectra allowing simple and definitive identification from other translucent phases found in many hypersaline fluid inclusions. Although currently only identified from a limited number of occurrences, given the availability of a definitive means of identification, we suspect that ramanite-(Rb) and ramanite-(Cs) may in fact be common, at least in boron-rich pegmatites.

Key Words: Fluid and melt inclusions • strong enrichment of boron • rubidium • cesium • Raman spectroscopy • new Cs and Rb minerals • ramanite-(Cs) • ramanite-(Rb)







JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Mineralogical Society of America