Abstract
Trace elements were determined for 12 celadonite and smectite-rich veins. The oxidative alteration zones have celadonite and Fe-oxyhydroxide and concentrations of K, Rb and B. The non-oxidative zones have Mg-rich smectite (saponite), talc and calcite plus high Li. Apparently, the smectite is enriched with Ni whose source was olivine in the basalt.-K.A.R.
| Original language | English (US) |
|---|---|
| Pages (from-to) | 491-497 |
| Number of pages | 7 |
| Journal | Initial Reports of the D.S.D.P. |
| Volume | 92 |
| State | Published - 1986 |