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Chapter 25. Arsenates, arsenites, phosphates, and vanadates |
 | | Although the number of arsenate, arsenite, phosphate, and vanadate species is second only to that of the silicates, specimens are for the most part rare, and many exceedingly so. |
 | | These species are almost entirely arsenates except magnussonite, nelenite, and schallerite, which are vein-filling arsenites; pyrobelonite and descloizite, which are the only known local vanadate minerals; and three anomalous and aberrant phosphates, meta-ankoleite, newberyite, and niahite. |
 | | The preponderance of the Sterling Hill arsenates are associated with zincite-bearing ore, the red-willemite ore of Parker and Troy (1982), in which no arsenic-bearing primary mineral is found; arsenic may have been introduced to this ore from the fl- willemite zone, the enclosing marble, or some other source. |
| franklin-sterlinghill.com /dunn/ch25/arsenates.stm (533 words) |
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