Abstract
Chemical and modal analyses of 22 partially serpentinized dunites from the Webster-Addie ultramafic body in North Carolina suggests losses of Mg and Fe, additions of Si and Na, and an increase in volume during progressive serpentinization of the dunites.
| Original language | English |
|---|---|
| Pages (from-to) | 1173-1179 |
| Number of pages | 7 |
| Journal | American Mineralogist |
| Volume | 54 |
| Issue number | 7-8 |
| Publication status | Published - Jul 1969 |
| Externally published | Yes |