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Hallimondite, a new uranium mineral from the Michael Mine near Reichenbach (Black Forest, Germany)
The hallimondite occurs as small tabular crystals with triclinic symmetry and as fine-grained coatings in cavities and fissures in quartz, in association with hügelite and mimetite. Data on mode of occurrence, crystallography, and physical, optical, chemical, and x-ray properties are reported. The f...
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Published in: | The American mineralogist 1965, Vol.50 (9), p.1143-1157 |
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Main Author: | |
Format: | Article |
Language: | English |
Subjects: | |
Online Access: | Get full text |
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Summary: | The hallimondite occurs as small tabular crystals with triclinic symmetry and as fine-grained coatings in cavities and fissures in quartz, in association with hügelite and mimetite. Data on mode of occurrence, crystallography, and physical, optical, chemical, and x-ray properties are reported. The formula Pb2(UO2)(AsO4)2 was derived from synthetic material. Comparison with the lead uranyl phosphate mineral parsonsite shows hallimondite to be the arsenate analogue of parsonsite. |
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ISSN: | 0003-004X 1945-3027 |