EVIDENCE FOR LATE PALEOCENE TO LATE EOCENE SEAFLOOR IN THE SOUTHERN NEW-HEBRIDES BASIN
We interpret marine magnetic anomaly data from the southern part of the New Hebrides basin as showing that a fragment of Late Paleocene-Late Eocene oceanic crust is preserved between the New Caledonia-Loyalty Islands platform and the New Hebrides island arc-trench system. The magnetic lineations whi...
| Autori principali: | , , |
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| Natura: | Journal article |
| Lingua: | English |
| Pubblicazione: |
1982
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