Hostname: page-component-cd9895bd7-gvvz8 Total loading time: 0 Render date: 2024-12-25T04:50:52.208Z Has data issue: false hasContentIssue false

Ferri-fluoro-katophorite from Bear Lake diggings, Bancroft area, Ontario, Canada: a new species of amphibole, ideally Na(NaCa)(Mg4Fe3+)(Si7Al)O22F2

Published online by Cambridge University Press:  02 July 2018

Roberta Oberti*
Affiliation:
CNR-Istituto di Geoscienze e Georisorse, Sede secondaria di Pavia, via Ferrata 1, I-27100 Pavia, Italy
Massimo Boiocchi
Affiliation:
Centro Grandi Strumenti, Università di Pavia, via Bassi 21, I-27100 Pavia, Italy
Frank C. Hawthorne
Affiliation:
Department of Geological Sciences, University of Manitoba, Winnipeg, Manitoba, R3T 2N2, Canada
Neil A. Ball
Affiliation:
Department of Geological Sciences, University of Manitoba, Winnipeg, Manitoba, R3T 2N2, Canada
Robert F. Martin
Affiliation:
Department of Earth and Planetary Sciences, McGill University, 3450. University Street, Montreal, Quebec H3A 2A7, Canada
*
*Author for correspondence: Roberta Oberti, Email: [email protected]

Abstract

Ferri-fluoro-katophorite is the second species characterised involving the rootname katophorite in the sodium–calcium subgroup of the amphibole supergroup. The mineral and its name were approved by the International Mineralogical Association Commission on New Minerals, Nomenclature and Classification, IMA2015-096. It was found in the Bear Lake diggings, Bancroft area, Ontario, Canada, where coarse euhedral crystals of amphibole, phlogopite, sanidine solid-solution (now coarsely exsolved to microcline perthite), titanite, augite, zircon and fluorapatite crystallised from a low-viscosity silicocarbonatitic magma of crustal origin. Greenish grey prismatic crystals of ferri-fluoro-katophorite generally protrude from the walls into a body of coarsely crystalline calcite, but they also occur away from the walls, completely enclosed by calcite. The empirical formula derived from electron microprobe analysis and single-crystal structure refinement is: A(Na0.55K0.32)Σ0.87B(Na0.79Ca1.18Mn2+0.03)Σ2.00C(Mg3.29Mn2+0.02Fe2+1.19Fe3+0.31Al0.09Ti4+0.08Li0.02)Σ5.00T(Si7.39Al0.61)Σ8.00O22W[F1.23 (OH)0.77]Σ2.00. Ferri-fluoro-katophorite is biaxial (–), with α = 1.640(2), β = 1.652(2), γ = 1.658(2), 2Vmeas. = 68.9(2)° and 2Vcalc.. = 70.1°. The unit-cell parameters are a = 9.887(3), b = 18.023(9), c = 5.292(2) Å, β = 104.66(3)°, V = 912.3(6) Å3, Z = 2 and space group C2/m. The strongest ten lines in the powder X-ray pattern [d values (in Å) I (hkl)] are: 2.708, 100, (151); 2.388, 74, (131); 3.139, 72, (310); 8.449, 69, (110); 2.540, 65, ($\bar{2}$02); 2.591, 53, (061); 2.739, 47, ($\bar{3}$31); 2.165, 45, (261); 3.279, 44, ($\bar{2}$40); 2.341, 43, ($\bar{3}$51).

Type
Article
Copyright
Copyright © Mineralogical Society of Great Britain and Ireland 2018 

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

Footnotes

Associate Editor: Ian Graham

References

Anovitz, L.M. and Essene, E.J. (1990) Thermobarometry and pressure-temperature paths in the Grenville Province of Ontario. Journal of Petrology, 31, 197241.Google Scholar
Armstrong, H.S. and Gittins, J. (1968) Geology of Glamorgan and Monmouth Townships, Haliburton County. Ontario Geological Survey, Open-File Report 5021.Google Scholar
Bartelmehs, K.L., Bloss, F.D., Downs, R.T. and Birch, J.B. (1992) EXCALIBR II. Zeitschrift für Kristallographie, 199, 185196.Google Scholar
Bruker (2003) SAINT Software Reference Manual. Version 6. Bruker AXS Inc., Madison, Wisconsin, USA.Google Scholar
Burke, A.J. and Leake, B.E. (2004) Named amphiboles: a new category of amphiboles recognized by the international Mineralogical Association (IMA), and the proper order of prefixes to be used in amphibole names. The Canadian Mineralogist, 42, 18811884.Google Scholar
Hawthorne, F.C., Ungaretti, L. and Oberti, R. (1995) Site populations in minerals: terminology and presentation of results of crystal-structure refinement. The Canadian Mineralogist, 33, 907911.Google Scholar
Hawthorne, F.C., Oberti, R. and Martin, R.F. (2006) Short-range order in amphiboles from the Bear Lake diggings, Ontario. The Canadian Mineralogist, 44, 11711179.Google Scholar
Hawthorne, F.C., Oberti, R., Harlow, G.E., Maresch, W.V., Martin, R.F., Schumacher, J.C. and Welch, M.D. (2012) Nomenclature of the amphibole supergroup. American Mineralogist, 97, 20312048.Google Scholar
Mandarino, J.A. (1981) The Gladstone-Dale relationship: Part lV. The compatibility concept and its application. The Canadian Mineralogist, 19, 441450.Google Scholar
McLelland, J.M., Selleck, B.W., Hamilton, M.A. and Bickford, M.E. (2010) Late- to post-tectonic setting of some major Proterozoic anorthosite – mangerite – charnockite – granite (AMCG) suites. The Canadian Mineralogist, 48, 729750.Google Scholar
North, A.C.T., Phillips, D.C. and Mathews, F.S. (1968) A semi-empirical method of absorption correction. Acta Crystallographica, A24, 351359.Google Scholar
Oberti, R., Ungaretti, L., Cannillo, E. and Hawthorne, F.C. (1992) The behaviour of Ti in amphiboles: I. Four- and six-coordinated Ti in richterites. European Journal of Mineralogy, 4, 425439.Google Scholar
Oberti, R., Hawthorne, F.C., Cannillo, E. and Cámara, F. (2007) Long-range order in amphiboles. Pp. 125172 in: Amphiboles: Crystal Chemistry, Occurrence and Health Issues (Hawthorne, F.C., Oberti, R., Della Ventura, G. and Mottana, A., editors). Reviews in Mineralogy and Geochemistry, 67. The Mineralogical Society of America and the Geochemical Society, Chantilly, Virginia, USA.Google Scholar
Oberti, R., Boiocchi, M., Hawthorne, F.C., Ball, N.A. and Harlow, G.E. (2015) Katophorite from the Jade Mine Tract, Myanmar: mineral description of a rare (grandfathered) end-member of the amphibole supergroup. Mineralogical Magazine, 79, 355363.Google Scholar
Ottolini, L., Bottazzi, P. and Vannucci, R. (1993) Quantification of lithium, berillium and boron in silicates by secondary ion mass spectrometry using conventional energy filtering. Analytical Chemistry, 65, 19601968.Google Scholar
Pushcharovski, D.Y., Lebedeva, Y.S., Pekov, I.V., Ferraris, G., Novakova, A.A. and Ivaldi, G. (2003) Crystal structure of magnesioferrikatophorite. Crystallographic Reports, 48, 1623.Google Scholar
Robinson, K., Gibbs, G.V. and Ribbe, P.H. (1971) Quadratic elongation: a quantitative measure of distortion in coordination polyhedra. Science, 172, 567570.Google Scholar
Streepey, M.M., Essene, E.J. and Van der Pluijm, B.A. (1997) A compilation of thermobarometric data from the Metasedimentary Belt of the Grenville Province, Ontario and New York State. The Canadian Mineralogist, 35, 12371247.Google Scholar
Vertolli, V., Back, M., Fouts, C. and Mandarino, J. (1998) Mineralogy of Bancroft, Ontario. International Mineralogical Association, 17th General Meeting (Toronto), Field Trip B5.Google Scholar
Supplementary material: File

Oberti et al. supplementary material

Oberti et al. supplementary material 1

Download Oberti et al. supplementary material(File)
File 15.6 KB