HR: 0800h
AN: V41C-1459    [Abstracts]
TI: The Pacific-Antarctic Ridge Between 41deg S: hot Underlying Mantle Evidenced by Bathymetry and Gravity Studies Coupled to Geochemical Results.
AU: Ondreas, H
EM: helene.ondreas@ifremer.fr
AF: IFREMER, BP 70, Plouzane, 29280 France
AU: * Klingelhoefer, F
EM: fklingel@ifremer.fr
AF: IFREMER, BP 70, Plouzane, 29280 France
AU: Briais, A
EM: Anne.Briais@dtp.obs-mip.fr
AF: CNRS, UMR 5562, OMP, 14, Ave. E. Belin, Toulouse, 31400 France
AU: Hamelin, C
EM: ced.hamelin@yahoo.fr
AF: IUEM, Place Copernic, Plouzane, 29280 France
AU: Dosso, L
EM: laure@ifremer.fr
AF: CNRS, UMR 6538, BP 70, Plouzane, 29280 France
AB: During the PACANTARCTIC 2 cruise, from December 17, 2004 to January 17, 2005, onboard the French research vessel L'Atalante, the geomorphology of the Pacific-Antarctic Ridge was mapped using EM12 multibeam bathymetry and imagery between 53° and 41° S together with along axis gravity measurements and dredges. The ridge axis generally deepens in this region from the south towards the north. Analysis of the bathymetric, gravity and geochemical data reveal, south of the Menard Fracture Zone, three distinct ridge segments (S1-S3) respectively 220, 100 and 120 km-long from south to north, separated by non transform discontinuities. From the north of the fracture zone to 41°S, five segments (N1-N5), 110 to 260 km-long, are present. Two segments (S2 and N2) seem to be transitional segments between fully developed and more robust ones. Calculation of the cross-sectional area from the bathymetric data allows quantification of the variation in size of the central bathymetric anomaly. It yields information about the inflation of the ridge and therefore its magmatic-tectonic state. The mantle Bouguer anomaly can be calculated by subtracting the gravity anomaly predicted from a model which includes the seafloor bathymetry and a simple one layer crustal model from the observed free-air gravity anomaly. It provides information about regions of anomalous mantle temperature or crustal thickness. Both parameters (cross-sectional area and mantle Bouguer anomaly) give evidence that two segments of the ridge at 49°S and 50°S near major off-axis volcanoes on each part of the Menard FZ are underlain by anomalously hot mantle. At these places, the dome is robust, reaching 10 km in width, 400 m in height, 2200m in depth south of Menard FZ and 8 km in width, 300 m in height and 2300 in depth north of Menard FZ. Geochemical analyses of samples dredged during the survey show a close correlation of high cross-sectional area values, positive mantle Bouguer anomalies with enriched volcanism along the two segments of the axis close to the Menard Fracture zone.
DE: 1021 Composition of the oceanic crust
DE: 1032 Mid-oceanic ridge processes (3614, 8416)
DE: 1219 Gravity anomalies and Earth structure (0920, 7205, 7240)
DE: 3038 Oceanic plateaus and microcontinents
DE: 3075 Submarine tectonics and volcanism
SC: Volcanology, Geochemistry, Petrology [V]
MN: Fall Meeting 2005