Articles | Volume 37, issue 5
https://doi.org/10.5194/ejm-37-819-2025
https://doi.org/10.5194/ejm-37-819-2025
Research article
 | 
23 Oct 2025
Research article |  | 23 Oct 2025

The M2(PO4)2Φ8 cyclic tetramer – a flexible structure-building unit – Part 1: Primary pegmatite phosphate minerals

Ian Edward Grey

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Cited articles

Baur, W. H.: Zur Kristallchemie der Salzhydrate. Die Kristallstrukturen von MgSO4.4H2O (Leonhardtit) und FeSO4.4H2O (Rozenit), Acta Crystallogr., 15, 815–826, 1962. 
Calvo, C.: The crystal structure of graftonite, Am. Mineral., 53, 742–750, 1968. 
de Wit, F. and Mills, S. J.: Arrojadite-group nomenclature: sigismundite reinstated, Eur. J. Mineral., 34, 321–324, https://doi.org/10.5194/ejm-34-321-2022, 2022. 
Dowty, E.: ATOMS for Windows, vsn. 6.1. Shape Software, Kingsport, USA, 2004.  
Fleck, M. and Kolitsch, U.: Natural and synthetic compounds with krohnkite-type chains. An update, Z. Kristallogr., 218, 553–567, 2003. 
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Short summary
The paper describes an analysis of the crystal structures of the minerals of the triphylite, alluaudite, zwieselite, and graftonite groups, from the perspective of the ubiquitous presence of 2-polyhedra-wide ribbons formed from corner linking of M2(PO4)2Φ8 cyclic tetramers. The study helps to unify the crystal chemistry of the four most dominant primary Fe and Mn phosphate mineral groups in granitic pegmatites.
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