Abstract
Pumpellyite occurs as radiating crystals in cavities in altered syenite from the Prospect Intrusion near Sydney, New South Wales, with a variety of other minerals. Optically positive and negative pumpellyite coexist, and the optical properties show no correlation with mineral association. The vavity-filling minerals grew at low temperature and confining pressure.
| Original language | English |
|---|---|
| Pages (from-to) | 320-324 |
| Number of pages | 5 |
| Journal | American Mineralogist |
| Volume | 54 |
| Issue number | 1-2 |
| Publication status | Published - Jan 1969 |
| Externally published | Yes |