Lateral heterogeneity in the seismic structure of the oceanic crust inferred from velocity studies in the Bay of Islands ophiolite, Newfoundland
In the Bay of Islands ophiolite complex of Western Newfoundland, Lower Ordovician crust and upper mantle are exposed in four massifs. Two of these, the Blow-Me-Down and North Arm massifs, contain complete or nearly complete ophiolite successions ranging from clastic sediments at the top, through pil...
Published in: | Geophysical Journal International |
---|---|
Main Authors: | , |
Format: | Text |
Language: | English |
Published: |
Oxford University Press
1982
|
Subjects: | |
Online Access: | http://gji.oxfordjournals.org/cgi/content/short/68/3/675 https://doi.org/10.1111/j.1365-246X.1982.tb04922.x |