1. The Rose Road Localities, Town of Pitcairn, St. Lawrence County New York: Part 5—Special Topics.
- Author
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Chamberlain, Steven C., Walter, Michael R., Bailey, David G., Emproto, Christopher R., Robinson, George W., Chiarenzelli, Jeffrey R., and Lupulescu, Marian
- Subjects
MINERALS ,CALCITE crystals ,PHLOGOPITE ,CORDIERITE ,FLUORAPATITE ,ROSES ,GOLD ores - Abstract
The wollastonite and resulting pseudomorphs are fairly sharply crystallized and occur either as isolated crystals in areas of coarsely crystallized calcite or as crystals lining the walls of a diopside-albite rock that faces into coarsely crystallized calcite. PSEUDOMORPHS Wollastonite Skarn (WSK) Almost all the pseudomorphs observed at the WSK are alterations or replacements of primary wollastonite. A detailed preliminary study concluded that the original mineral was unlikely to be nepheline but could have been cordierite, based on the presence of crystallized quartz in the mineral assemblage of the occurrence and the likelihood from contact goniometry that the original mineral was orthorhombic rather than hexagonal. The following observations support our conclusion that these pseudomorphs resulted from later alteration of preexisting meionite crystals: We have observed no marialite crystals without a meionite core. [Extracted from the article]
- Published
- 2022
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