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- W2049674089 abstract "The structure and evolution of the Kerguelen-Heard Plateau, the northern domain of the Kerguelen-Gaussberg Ridge, is derived from stratigraphic interpretation of multichannel seismic profiles. The Kerguelen-Heard Plateau was created between 130 and 100 Ma at or near an active spreading center in the gap between the Antarctica-Australia plate and the India plate. From the early Late Cretaceous (about 100 Ma) to the Eocene (42–45 Ma) the Kerguelen-Heard Plateau was a shallow marine structure continuously subsiding at a rate of about 20 m Ma−1 and covered by pelagic and shelf sediments. At 42–45 Ma the Kerguelen-Heard Plateau and Broken Ridge were clearly separated by sea-floor spreading at the Southeast Indian Ridge. From 42–45 Ma to the Miocene, a major gap of sedimentation occurred. Later the Kerguelen-Heard Plateau was covered by pelagic sediments, interbedded with thick clastic sedimentary layers coming essentially from Kerguelen Island." @default.
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- W2049674089 date "1987-01-01" @default.
- W2049674089 modified "2023-09-30" @default.
- W2049674089 title "Structure and evolution of the Kerguelen-Heard Plateau (Indian Ocean) deduced from seismic stratigraphy studies" @default.
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- W2049674089 doi "https://doi.org/10.1016/0025-3227(87)90022-3" @default.
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