Scheduled Cruises in 2003
Summary of a scheduled cruise on margins research
(ODP.031)
Newfoundland margin, N. Atlantic
DV Joides
Resolution (Leg 210)
10 July 2003 from : Bermuda
9 September 200 in : St John’s,
Newfoundland
Jean-Claude
Sibuet, Brian Tucholke
Ocean Drilling Program, College
Station, Texas, USA
aklaus@odpemail.tamu.edu
Drilling on the
Iberian margin has documented extreme extension with little or no
decompression melting of the asthenospheric mantle. Observations from
geophysical studies on the conjugate Newfoundland margin document
significant cross-rift asymmetries in basement depth, amount of
tectonic extension, and other deep structures. These observations raise
fundamental questions about rifting of non-volcanic margins, including
the cause and extent of mantle unroofing, the presence or absence of
decompression melting, the origin of deep and crustal asymmetry between
conjugates, the age-subsidence and strain partitioning history, and the
relation of rift events to development of shallow water unconformities
and the stratigraphic record. Leg 210 will study the composition and
subsidence history of the stratigraphic sequence above basement and
igneous/tectonic basement contact on the Newfoundland margin. The
proposed drilling is in a position exactly conjugate to the Iberia
abyssal plain drilling transect.
The single reentry site is located in 4559 m water depth. A pilot hole
will be cored in soft sediments to ~500 mbsf. A second hole will be
cored and logged to 1500 m, following which it will cored as deep as
possible in the time remaining with a target of 2200 m in sediment with
100 m of basement penetration. The sedimentary sequence is expected to
consist of detrital sediments, principally clays and silty clays, with
limestone beds and lenses.
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