Scheduled Cruises in 2003
Summary of a recent cruise on margins research (CA.031)
Davis Strait, N Labrador Sea
CCGS Hudson
(NEON)
10th August, 2003; Dartmouth, NS, Canada
2nd September, 2003; Dartmouth, NS, Canada
Thomas Funck
Danish Lithosphere Centre, Copenhagen,
Denmark
H. Ruth Jackson, Geological
Survey of Canada (Atlantic Division), Dartmouth, Nova Scotia, Canada;
Keith E. Louden, Department of Oceanography, Dalhousie University,
Halifax, Nova Scotia, Canada
tf@dlc.ku.dk
Understanding the
crustal structure within Davis Strait is critical for assessing
mantle plume dynamics and the formation of transform margins.
The purpose of the wide-angle reflection/refraction seismic study is to
determine the nature of the crust in the
southern Davis Strait at the transition from the non-volcanic style
continental margins in the Labrador Sea to
the volcanic transform-rifted margin between Baffin Island (Canada) and
West Greenland. Previous studies are
mainly based on multichannel reflection seismic and magnetic data and
result in conflicting interpretations
with regard to the deeper crustal structure and the plate
reconstruction between Greenland and North America.
The two seismic refraction lines in Davis Strait will provide a
velocity model for the crust and uppermost mantle,
which will help to distinguish between crustal types (oceanic,
continental, transitional/serpentinized mantle).
This information puts constraints on the rifting history and plate
reconstruction.
Mapping of magmatic underplating and analysis of the deep crustal
structure of the large transform fault system
in the strait will show how the Greenland-Iceland mantle plume
interacted with the northward extent of the
Labrador Sea rift.
Transform faults in Davis Strait acted as leaky fracture zones but
their deep structure is not known.
In addition to the seismic experiment, several heat flow measurements
will be carried out.
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