HR: 0800h
AN: T11A-1231    [Abstracts]
TI: Franklin Volcanic Field: Characteristics of a Submarine Volcanic Province in the Western Ross Sea, Antarctica
AU: * Smith, A E
EM: smith.3915@osu.edu
AF: Dept. of Geological Sciences, Ohio State University, 125 S. Oval Mall, Columbus, OH 43210 United States
AU: Wilson, T J
EM: wilson.43@osu.edu
AF: Dept. of Geological Sciences, Ohio State University, 125 S. Oval Mall, Columbus, OH 43210 United States
AU: Davis, M
EM: marcyd@gbronline.com
AF: University of Texas Institute for Geophysics, 4412 Spicewood Springs Rd., Austin, TX 78759 United States
AU: Lawver, L A
EM: lawver@utig.ig.utexas.edu
AF: University of Texas Institute for Geophysics, 4412 Spicewood Springs Rd., Austin, TX 78759 United States
AU: Mukasa, S
EM: mukasa@umich.edu
AF: Dept. of Geological Sciences, University of Michigan, 2534 C.C. Little Bldg., Ann Arbor, MI 48109 United States
AB: The RVIB N. B. Palmer collected bathymetric and seismic data in the western Ross Sea in January/February 2004 with the specific purpose of mapping neotectonic structural and volcanic features on and beneath the seafloor. The Franklin Volcanic Field (FVF) is an important feature revealed by the bathymetric data. The volcanic field, which is expressed as a regional bathymetric high, is a minimum of 80 km long and up to 40 km wide. As one moves north, the overall trend of the volcanic field appears to curve from N-S to NE. Superimposed on the regional high are the subaerial portion of Franklin Island and clusters of submarine volcanic cones. Franklin Island has been interpreted as the western remnant of a shield volcano and has a single K-Ar date of 4.8+2 Ma. Its submarine morphology is characterized by a steep western flank and an eastern flank that, within the limits of the mapped region, appears to have a shallower slope. South of Franklin Island there is a cluster of cones which lead into the steep southern slope. North of the island, there are at least 7 discrete cones. Five of the volcanic cones in the FVF were dredged, yielding basaltic lava, hyaloclastite and tuff. Abundant glass is preserved in the volcanics, some lavas are olivine-phyric, and lavas locally contain mantle and crustal xenoliths. The seafloor morphology in the northern sector of the field is characterized by lineations at several scales, some hummocky terrain marked by circular to oval depressions, and superimposed iceberg scours. Based on morphology alone, the linear features could reflect volcanic ridges, faults, current or glacial lineations, or may have formed by a combination of these processes. The origin of the seafloor features within the FVF is being determined through integrated analysis of magnetic, gravimetric and seismic data. When genesis is established, regional and local feature trends will be used to interpret the direction of glacial flow as well as maximum and minimum crustal stress directions at the time of formation of the FVF.
DE: 8400 VOLCANOLOGY
DE: 9310 Antarctica
DE: 8107 Continental neotectonics
DE: 8109 Continental tectonics--extensional (0905)
DE: 8164 Stresses--crust and lithosphere
SC: Tectonophysics [T]
MN: 2004 AGU Fall Meeting