Scheduled Cruises in 2003
Summary of a scheduled cruise on margins research (UK.031)
NW Indian Ocean
RRS Charles Darwin 144
13 January 2003 from: Muscat, Oman
22 February 2003 in: Mahé, Seychelles
JS Collier
Imperial College,
University of London, UK
M Kendall,
PR Miles, T Minshull, RB Whitmarsh
jenny.collier@ic.ac.uk
We collected a comprehensive normal incidence and wide-angle seismic
dataset to determine
the deep structure and rift architecture of a conjugate pair of
continental margins where initial spreading rate was fast
(> 50 mm/yr) i.e. the north Seychelles and Laxmi Ridge margins. The
results will be compared to predictions from
numerical models to validate the models and improve our understanding
of continental rifting and breakup. Numerical
models developed to explain the magmatic and tectonic behaviour of
rifted continental margins have been heavily
influenced by observations made at margins where the initial seafloor
spreading rate was slow (<25 mm/yr half rate).
Further, the models have been devised largely to match observations
from just one side of the continental rift which may
or may not be representative of the conjugate rifted margin. We also
collected gravity, magnetic, 3.5 kHz and
swath-bathymetry profiles and obtained rocks from two dredge hauls on
the N Seychelles margin.
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