Abstract
This work confirms earlier suggestions that regional 18O depletion patterns in areas of dominantly silicic magmatism coincide with epithermal districts and indicates their value as exploration tool. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 662-673 |
| Number of pages | 12 |
| Journal | Economic Geology |
| Volume | 89 |
| Issue number | 3 |
| DOIs | |
| Publication status | Published - 1994 |
| Externally published | Yes |
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