A seismic refraction transect across the Galicia Bank continental margin shows that the original continental crust thins westward from 17 to 2 km immediately east of a margin‐parallel peridotite ridge (PR). Immediately west of the PR, oceanic crust is only 2.5–3.5 km thick, but farther west (oceanwa...
Research Assistant
AI chat, annotations, notes & similar papers
No comments yet
Be the first to share your thoughts!