<?xml version="1.0"?>
<oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:title>Deep structure of the southern Kerguelen Plateau (southern Indian Ocean) from ocean bottom seismometer wide-angle seismic data</dc:title>
  <dc:creator>Operto, D.</dc:creator>
  <dc:creator>/Charvis, Philippe</dc:creator>
  <dc:description>Wide-angle seismic data collected during the Kerguelen ocean bottom seismometer experiment provide the first images of the deep structure of the southern Kerguelen Plateau and support a new interpretation of the origin of the plateau. Velocity models based on travel time inversions and reflectivity synthetic seismograms show a 22-km-thick crust composed of average 1.6 km of sedimentary cover, average 5.3 km of upper crust, average 11.0 km of lower crust, and a 4- to 6-km-thick reflective zone immediately above Moho. Velocities in the upper crust (from 3.8-4.5 km/s at top to 6.0-6.5 km/s at bottom) are consistent with the basaltic nature of this layer, the top of which was sampled during the Ocean Drilling Program. Velocities in the lower crust increase continuously from 6.60 km/s at the top to 6.90 km/s at 19.5 km depth. The reflective zone at the base of the crust identified by wide-angle reflections is observed only along the NNW-SSE direction. It consists of alternating high- and low-velocity layers with an average velocity of 6.70 km/s in the NNW-SSE direction and ?6.90 km/s in the perpendicular direction. Strong azimuthal anisotropy is also observed in the upper mantle with velocities of 8.60 and 8.00 km/s, in the NNW-SSE and E-W directions, respectively. The absence of high velocities at the base of the crust that characterizes many large-volume mafic provinces, the reflective lower crust, and anisotropy in upper mantle suggest that the southern Kerguelen Plateau represents a stretched continental fragment overlain by basaltic flows isolated from the Antarctic margin during the early opening of the Indian Ocean</dc:description>
  <dc:date>1996</dc:date>
  <dc:type>text</dc:type>
  <dc:identifier>https://www.documentation.ird.fr/hor/fdi:010083753</dc:identifier>
  <dc:identifier>fdi:010083753</dc:identifier>
  <dc:identifier>Operto D., Charvis Philippe. Deep structure of the southern Kerguelen Plateau (southern Indian Ocean) from ocean bottom seismometer wide-angle seismic data. 1996, 101 (B11), 25077-25103</dc:identifier>
  <dc:language>EN</dc:language>
  <dc:coverage>KERGUELEN</dc:coverage>
  <dc:coverage>OCEAN INDIEN</dc:coverage>
</oai_dc:dc>
