Summary
Childrenite and crandallite are described as two new phosphate members in the paragenesis of the Stari Trg mine which comprises vivianite, ludlamite and struvite. Crandallite crystals with very simple rhombohedral habit grow on rhombohedral carbonate and childrenite crystals. The crystal morphology of childrenite is very similar to that at described from other localities. Following forms were measured: {100}, {100}, {110}, {120}, {121}, {221} and {342}. The average chemical composition is Ch91 Eo9 (Ch-childrenite, Eo-eosphorite). Pseudo-orthorhombic unit cell dimensions were calculated: a = 10.390(4) A, b = 13.390(4) A and c = 6.920(2) A. Growth sectors and sector twins of childrenite are described.
Zusammenfassung
Childrenit und Crandallit werden als zwei neue Minerale der Phosphatgruppe beschrieben. Sie stammen aus der Stari Trg Grube in Paragenese mit Vivianit, Ludlamit und Struvit. Die Crandallit-Kristalle mit einfachem rhomboedrischen Habitus, wachsen rhomboedrischen Karbonat- und Childrenit-Kristallen auf. Die Kristallmorphologie von Childrenit ist, verglichen mit der aus anderen Lokalitäten, sehr einfach. Folgende Formen wurden gemessen: {100}, {010}, {110}, {120}, {121}, {221} und {342}. Die durchschnittliche chemische Zusammensetzung ist Ch(91Eo9(Ch-Childrenit, Eo Eosphorit). Eine Kalkulation der pseudo-orthorhombischen Elementarzelle ergab folgende Abmessungen: a = 10.390(4) A, b = 13.390(4) A and c = 6.920(2) A. Schließlich wird das Wachstum and die Zwillingsbildung von Childrenit beschrieben.
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Bermanec, V., Šćavničar, S. & ZebeC, V. Childrenite and crandallite from the Stari Trg mine (Trepča), Kosovo: new data. Mineralogy and Petrology 52, 197–208 (1995). https://doi.org/10.1007/BF01163245
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DOI: https://doi.org/10.1007/BF01163245