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- W1543071421 abstract "The few rock outcrops on Adelie Coast-Wilkes Land consist mainly of Precambrian plutonic rocks and metasediments. On the continental margin, several multichannel seismic surveys, including the 1982 IFP survey, reveal the presence of a thick sedimentary basin, especially beneath the outer continental shelf and upper slope, where it may exceed 6000 m. Thin basin results from the creation and evolution of a continental margin, initiated some 100 Ma from the separation of Australia and Antarctica. Beneath the outer shelf, which is 400-500 m deep, the sedimentary series consist of four units separated by three major unconformities: (1) a predrift unit including a Precambrian basement, possible Paleozoic and early Mesozoic sediments, and a Mesozoic syn-rift sequence; (2) an upper Eocene to Oligocene unit in a shallow marine environment; and (3) a Neogene glacial prograding unit. The predrift and early postrift units are considered to be a promising target with reference to other passive margins, although no major hydrocarbon accumulation has been discovered as yet on the Australian conjugate margin." @default.
- W1543071421 created "2016-06-24" @default.
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- W1543071421 date "1990-01-01" @default.
- W1543071421 modified "2023-09-23" @default.
- W1543071421 title "Geology and Petroleum Potential of the Adelie Coast Margin, East Antarctica" @default.
- W1543071421 doi "https://doi.org/10.1306/st31524c6" @default.
- W1543071421 hasPublicationYear "1990" @default.
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