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Geology and petroleum potential of Adelie Coast margin, east Antarctica

Conference · · AAPG (Am. Assoc. Pet. Geol.) Bull.; (United States)
OSTI ID:5999219
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.
Research Organization:
Institut Francais du Petrole, Rueil Malmaison, France
OSTI ID:
5999219
Report Number(s):
CONF-870606-
Conference Information:
Journal Name: AAPG (Am. Assoc. Pet. Geol.) Bull.; (United States) Journal Volume: 71:5
Country of Publication:
United States
Language:
English

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