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Mineralogical Magazine; April 2004; v. 68; no. 2; p. 231-240; DOI: 10.1180/0026461046820183
© Mineralogical Society of Great Britain and Ireland
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FIG. 3. Polyhedral representation of the structure of petewilliamsite. MOn polyhedra are shaded with parallel lines, and arsenate tetrahedra are shaded solid grey.





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JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
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