Scheduled Cruises in 2001
Summary of a recent cruise on margins research (CA.011)
off Nova Scotia, Canada
CCGS Hudson
(SMART)
20th June, 2001; Dartmouth, NS, Canada
11th July, 2001; Dartmouth, NS, Canada
Keith E. Louden
Department of Oceanography, Dalhousie
University, Halifax, Nova Scotia, Canada
H. Ruth Jackson and Sonya A.
Dehler, Geological Survey of Canada (Atlantic Division), Dartmouth,
Nova Scotia, Canada
Keith.Louden@Dal.Ca
The continental margin
off Nova Scotia, Canada, marks the transition from volcanic style
margins to the south (U.S. East coast) to non-volcanic style margins to
the north (Newfoundland and Labrador). Off Nova Scotia, the East Coast
Magnetic Anomaly (ECMA) progressively weakens northward and eventually
disappears. A well developed ECMA commonly correlates with seaward
dipping reflections (SDR). The SMART refraction seismic experiment was
designed to study the transition from volcanic to non-volcanic style
margins. Data were collected along three lines covering the entire
transition zone. The southernmost line lies within the area where
seaward dipping reflectors are observed, while the northernmost line is
located just north of where the ECMA disappears.
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