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...

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Bibliographic Details
Published in:Geophysical Journal International
Main Authors: Christensen, Nikolas I., Salisbury, Matthew H.
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