A geophysical investigation of the nova scotian continental shelf

A major east-west structural discontinuity, termed the Minas Basin - Chedabucto Bay - Orpheus fault zone, transects Nova Scotia and the adjacent Nova Scotian continental shelf. To the north of this discontinuity, the geophysical evidence indicates structural continuity between the late Precambrian b...

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Bibliographic Details
Main Author: Goodacre, Alan Kenneth
Format: Thesis
Language:unknown
Published: 1976
Subjects:
Breton Island
Newfoundland
Online Access:http://etheses.dur.ac.uk/8174/
http://etheses.dur.ac.uk/8174/1/8174_5174.PDF

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