HR: 1340h
AN: T13D-0503    [Abstracts]
TI: Tectonic evolution of the South Fiji Basin: UNCLOS helps tackle regional tectonics
AU: Herzer, R
EM: r.herzer@gns.cri.nz
AF: GNS Science, PO Box 30368, Lower Hutt, 6009 New Zealand
AU: Roest, W
EM: walter.roest@ifremer.fr
AF: IFREMER, Geosciences Marines, BP 70, Plouzane, 29280 France
AU: * Barker, D
EM: d.barker@gns.cri.nz
AF: GNS Science, PO Box 30368, Lower Hutt, 6009 New Zealand
AU: Mortimer, N
EM: n.mortimer@gns.cri.nz
AF: GNS Science, Private Bag 1930, Dunedin, 9001 New Zealand
AU: Mauffret, A
EM: alain.mauffret@lgs.jussieu.fr
AF: Univ. P. et M. Curie, Lab. Tectonique, 4 Place Jussieu, Paris, 75256 France
AU: Lafoy, Y
EM: yves.lafoy@gouv.nc
AF: Service de la Geologie et des Mines (SGM), Direction de l'Industrie, des Mines et de l'Energie de Nouvelle-Caledonie (DIMENC), BP 465, Noumea, 98845 New Caledonia
AB: Marine surveys to study the evolution of remnant arcs and backarc basins north of New Zealand have been complemented by UNCLOS surveys by three countries - France, New Zealand and Australia - with potential extended continental shelf claims in the region. The UNCLOS factor allowed 9 cruises to focus on the region in the past 9 years, collecting approximately 30,000 km of seismic reflection (5,000 deep crustal), 263,700 sq km of swath bathymetry, and 70 dredge samples. Feedback through sharing or publishing data and joint participation allowed efficient planning and deployment of academic and UNCLOS cruises. Two models for South Fiji (SFB) and Norfolk (NB) basin evolution arise from current studies: at the level of the Three Kings Ridge - NB - southern SFB both involve Pacific trench roll-back and southward propagating spreading, but one also uses two subduction systems and arc-continent collision. Linked spreading of the NB and SFB is invoked in both models, but the veracity and geodynamics of the link are not investigated. A growing body of petrological and radiometric evidence and the tectonics of the New Zealand continental margin point to tandem Early Miocene spreading of the SFB and NB despite published magnetic interpretations that would confine SFB spreading to the Oligocene. The Franco-NZ NOUCAPLAC-1 cruise, the last cruise relevant to UNCLOS in this region, included a scientific objective to investigate the SFB-NB link in the critical area bounded by the Loyalty Ridge (LR), the Cook Fracture Zone (CFZ), the Bounty spreading centre (BSC) and the Julia Lineament (JL) with swath mapping, magnetics and seismic reflection. Initial results show a complex bathymetry where a possible link between the BSC and the CFZ involves ridge propagation, overlapping spreading centres, rift blocks and overprinting volcanoes. The link to the JL was not adequately tested due to sparse coverage. Closer to the LR, a thick, faulted sedimentary basin was found.
DE: 3000 MARINE GEOLOGY AND GEOPHYSICS
DE: 3040 Plate tectonics (8150, 8155, 8157, 8158)
DE: 3045 Seafloor morphology, geology, and geophysics
SC: Tectonophysics [T]
MN: Fall Meeting 2005