Abstract
Habit, association, chemistry and manner of formation are analysed for glaucochroite, a member of the olivine group, known primarily from the Zn-Mn-Fe deposit at Franklin, New Jersey. Cuspidine, Ca4Si2O7(F,OH)2, is confirmed as occurring at Franklin. It occurs with glaucochroite and hardystonite, and in solution vugs in willemite.-J.A.Z.
Original language | English (US) |
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Pages (from-to) | 423-428 |
Number of pages | 6 |
Journal | American Mineralogist |
Volume | 72 |
Issue number | 3-4 |
State | Published - Jan 1 1987 |
Externally published | Yes |
ASJC Scopus subject areas
- Geophysics
- Geochemistry and Petrology