Geological Literature
The Troodos ophiolite was probably formed through subduction of an active mid-ocean ridge (I-3-26 P-16)(abs.)
OSOZAWA Soichi, OKAMURA Makoto
| item | description |
|---|---|
| Title | The Troodos ophiolite was probably formed through subduction of an active mid-ocean ridge (I-3-26 P-16)(abs.) |
| Authors | OSOZAWA Soichi, OKAMURA Makoto |
| Data name | Abstracts, 29th International Geological Congress |
| Volume | 1 |
| Page | 138-138 |
| Year | 1992 |
| Publisher | International Geological Congress (IGC) |
| Language | EN |
| @id | https://gbank.gsj.jp/ld/resource/geolis/199205946 |