Scheduled Cruises in 2000
Summary of a recent cruise on margins research (CA.001)
N. Atlantic, Newfoundland
non-volcanic rifted margin
R/V Maurice Ewing
EW0007
mid-July 2000 from St. Johns,
Newfoundland, Canada
late August 2000 in Newark, NJ, USA
R/V Oceanus
mid-July 2000 from St. Johns,
Newfoundland, Canada
late August 2000 in St. Johns,
Newfoundland, Canada
Woods Hole (WHOI), USA
Brian E. Tucholke, Woods Hole, USA
W. Steven Holbrook,
University of Wyoming, USA
Keith Louden, Dalhousie
University, CAN
John Hopper, GEOMAR, GER
Hans Christian Larsen, Danish
Lithosphere Centre, DEN
Sharon Deemer, Memorial
University of Newfoundland, CAN
Charles Hurich, Memorial
University of Newfoundland, CAN
Jeremy Hall, Memorial
University of Newfoundland, CAN
btucholke@whoi.edu
The purpose of the SCREECH (Studies of Continental
Rifting and Extension on the Eastern Canadian SHelf) program was to 1)
distinguish between competing hypotheses for the origin of crust
between
unambiguous oceanic and continental crust on the Newfoundland margin,
2)
to compare the crustal structure of the Newfoundland margin to the
conjugate Iberian margin in order to learn more about the processes
that
extend and ultimately rupture continental crust, and 3) to obtain site
survey data that could be used to select and justify ODP drill sites in
the Newfoundland Basin. To accomplish these objectives, coincident
multi-channel seismic (MCS) reflection data, wide-angle seismic
reflection/refraction data, gravity data and magnetic data were
collected
along three primary transects across the Newfoundland margin. Each
transect reached from unambiguous continental crust seaward past a
magnetic anomaly identified as M0, and thus onto presumed oceanic
crust.
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