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

American Mineralogist; June 1999; v. 84; no. 5-6; p. 773-777
This Article
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
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Galliski, M. A.
Right arrow Articles by Chapman, R.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Ferrotitanowodginite, Fe (super 2+) TiTa 2 O 8 , a new mineral of the wodginite group from the San Elias pegmatite, San Luis, Argentina

Miguel Angel Galliski, Petr Cerny, Maria Florencia Marquez-Zavalia, and Ron Chapman

Consejo Nacional de Investigaziones Cientificas e Technicas, Instituto Argentino de Nirologia, Glaciologia y Ciencias Ambientales, Mendoza, Argentina

Ferrotitanowodginite is a new mineral of the wodginite group, which is found in and defined from two closely adjacent pegmatites in the San Luis province, Argentina, but previously encountered in the Tanco (Manitoba) and Marko's (Ontario) pegmatites. In the San Elias pegmatite, ferrotitanowodginite occurs aggregated with ferrowodginite and associated with microlite, ferrotapiolite, cleavelandite, and quartz. In La Viquita pegmatite, ferrotitanowodginite occurs in a replacement unit associated with wodginite, ferrowodginite, titanowodginit and ferrotapiolite in yellow muscovite and quartz. Ferrotitanowodginite is very dark brown to black, with a dark brown streak and submetallic luster. Mohs hardness is 5 1/2 and D calc = 7.368 g/cm 3 . In reflected light, it is creamy white and gray in air and oil, respectively; anisotropy is distinct, bireflectance and pleochroism moderate. Ferrotitanowodginite is monoclinic, space group C2/c, Z = 4. Unit-cell dimensions for San Elias' material are a = 9.403(4) Aa, b = 11.384(3) Aa, c = 5.075(1) Aa, beta = 90.55 degrees (2) V = 543.24(22) Aa 3 . The strongest lines in the X-ray powder diffraction are d = 2.963 Aa, I = 100%, (hkl = 221); d = 2.939 Aa, I = 90% (hkl = 221); d = 3.626 Aa, I = 70% (hkl = 220); and d = 1.715 Aa, I = 50% (hkl = 402). Eighteen analyses by electron microprobe gave the following mean composition: WO 3 0.02, Nb 2 O 5 6.52, Ta 2 O 5 70.68, TiO 2 7.10, SnO 2 1.25, ThO 2 0.01, UO 2 0.02, As 2 O 3 0.03, Sb 2 O 3 0.02, Bi 2 O 3 0.03, Fe 2 O 3 2.18, MgO 0.01, CaO 0.01, MnO 1.05, FeO 10.27, PbO 0.05, total 99.25 wt%. The La Viquita sample is much richer in Mn and Sn. The simplified formula for ferrotitanowodginite is: (Fe (super 2+) , Mn (super 2+) ) (Ti,Sn (super 4+) , Ta,Fe (super 3+) ) (Ta,Nb) 2 O 8 , ideally Fe (super 2+) TiTa 2 O 8 .

This record provided courtesy of AGI/GeoRef.




This article has been cited by other articles:


Home page
Can MineralHome page
M. A. Galliski, M. F. Marquez-Zavalia, P. Cerny, V. A. Martinez, and R. Chapman
THE Ta-Nb-Sn-Ti OXIDE-MINERAL PARAGENESIS FROM LA VIQUITA, A SPODUMENE-BEARING RARE-ELEMENT GRANITIC PEGMATITE, SAN LUIS, ARGENTINA
Can Mineral, April 1, 2008; 46(2): 379 - 393.
[Abstract] [Full Text] [PDF]


Home page
Can MineralHome page
M. A. Galliski and P. Cerny
GEOCHEMISTRY AND STRUCTURAL STATE OF COLUMBITE-GROUP MINERALS IN GRANITIC PEGMATITES OF THE PAMPEAN RANGES, ARGENTINA
Can Mineral, June 1, 2006; 44(3): 645 - 666.
[Abstract] [Full Text] [PDF]


Home page
Can MineralHome page
P. Cerny and R. Chapman
EXSOLUTION AND BREAKDOWN OF SCANDIAN AND TUNGSTENIAN Nb Ta Ti Fe Mn PHASES IN NIOBIAN RUTILE
Can Mineral, February 1, 2001; 39(1): 93 - 101.
[Abstract] [Full Text] [PDF]




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