The Rietveld Refinement of Beryls from Pegmatitic System at Piława Górna, Góry Sowie Block, SW Poland

• Authors: S. Zelek-Pogudz , M. Zubko , A. Pieczka
• Languages of publication: EN

Abstracts

EN

The studied beryl crystals came from the Julianna pegmatitic system exposed in the Dolnośląskie Surowce Skalne S.A. quarry at Piława Górna. This mineral occurs here in various forms and colours (green, yellow, white, pinkish and blue) in almost all pegmatite bodies. The paper describes the relationship between the structure and chemical composition of different coloured beryl crystals.

Keywords

EN

91.65.An  

• Publisher: Institute of Physics, Polish Academy of Sciences
• Journal: Acta Physica Polonica A
• Year: 2016
• Volume: 130
• Issue: 4
• Pages: 898-900

Dates

published

2016-10

References

• [1] F.C. Hawthorne, M.A. Cooper, W.B. Simmons, A.U. Falster, B.M. Laurs, T. Armbruster, G.R. Rossman, A. Peretti, D. Günter, B. Grobéty, Mineral. Rec. 35, 369 (2004)
• [2] O.V. Yakubovich, I.V. Pekov, I.M. Steele, W. Massa, N.V. Chukanov, Crystallogr. Rep. 54, 399 (2009), doi: 10.1134/S1063774509030067
• [3] F.C. Hawthorne, P. Černý, Can. Mineral. 15, 414 (1977)
• [4] A. Pieczka, E. Szełęg, A. Szuszkiewicz, S. Ilnicki, K. Nejbert, K. Turniak, in: 7th Int. Symp. Granitic Pegmatites, PEG, Książ (Poland), 2015, Book of Abstracts, 75 (2015)
• [5] I.L. Pouchou, F. Pichoir, in: Microbeam Analysis, Ed. I.T. Armstrong, San Francisco Press, San Francisco 1985, p. 104
• [6] C. Aurisicchio, G. Fioravanti, O. Grubessi, P.F. Zanazzi, Am. Mineral. 73, 826 (1988)
• [7] J. Rodriguez-Carvajal, J. Phys. B 192, 55 (1993), doi: 10.1016/0921-4526(93)90108-I

Identifiers

DOI

10.12693/APhysPolA.130.898