HR: 1340h
AN: OS53A-0969 [Abstracts]
TI: A margin transformed: Pure extension to pure translation along the North Falklands Escarpment. Results of Article 76 surveying in the South Atlantic.
AU: * Parson, L M
EM: l.parson @noc.soton.ac.uk
AF: UNCLOS Group, National Oceanography Centre
European Way, Southampton, SO14 3ZH, United Kingdom
AU: Richards, P
AF: British Geological Survey, Kingsley Dunham Centre
Keyworth, Nottingham, NG12 5GG, United Kingdom
AU: Kimbell, G
EM: gsk@bgs.ac.uk
AF: British Geological Survey, Kingsley Dunham Centre
Keyworth, Nottingham, NG12 5GG, United Kingdom
AU: Maclachlan, I
AF: Petroleum Agency of South Africa, POBox 1174
Parow
7499, Parow, 7499, South Africa
AB:
The Falklands Plateau comprises an elongate continental block extending eastwards from the Falkland Islands
to the Maurice Ewing Bank, 900 kilometres away. While complicated by the transpressive convergence of the
Scotia Sea Plate in the South, its margin in the north is characterised by the extreme rectilinearity resulting from
its transform separation from the South African craton along the Agulhas Plateau/Ridge system. The translational
regime is flanked in the west by the well documented seaward dipping reflector sequences dominating the south
Argentine margin, but new and extensive swath bathymetric surveying along the escarpment reveals a transition
between the two opening modes characterised by a complex of sheared crustal segments, offset zones, and
transform discontinuities. Within this 60 km wide margin parallel zone, en echelon arrays of crustal ‘tears’,
many defining a crude tension gash geometry, host submarine elevations, which show varying degrees of
rotation in response to the increasing development of shear moment toward the east. We examine the tectonic
origin of the ridges in the context of the geological evolution of the margin, their connectivity to the margin, and the
comparison with the latest data from the conjugate Agulhas margin off South Africa.
DE: 4200 OCEANOGRAPHY: GENERAL
SC: Ocean Sciences [OS]
MN: 2007 Fall Meeting