Carbonate platform growth, demise and sea level record : Marion Plateau, Northeast Australia
Abstract
The Marion Plateau located between 18°S and approximately 23°S in the area beyond
the Great Barrier Reef offshore between Gladstone and Townsville is the most southerly
of the marginal plateaus in northeastern Australia. It forms a deeper extension of the
Queensland continental shelf with water depths ranging from 100m along its south
western margin to 500m along the northern and eastern margins. The plateau is bound
along its northern margin by the Townsville Trough; by the Cato Trough along the
eastern margin; and the central Great Barrier Reef to the south west. Modern reef
development on the Marion Plateau is confined to Marion Reef in the north and
Saumarez Reef in the south. The plateau is part of a slowly subsiding upper plate margin
and the plateau summit remained exposed throughout the Palaeogene during which
time it was planated to form a gently dipping relatively smooth plateau summit with a
maximum width of 200 km.
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