Evolution of three unconformity-bounded sandy carbonate successions in the McArthur River region of northern Australia: the Lawn, Wide and Doom Supersequences in a proximal part of the Isa Superbasin
Titel:
Evolution of three unconformity-bounded sandy carbonate successions in the McArthur River region of northern Australia: the Lawn, Wide and Doom Supersequences in a proximal part of the Isa Superbasin
Auteur:
Jackson, M. J. Southgate, P. N.
Verschenen in:
Australian journal of earth sciences
Paginering:
Jaargang 47 (2000) nr. 3 pagina's 625-635
Jaar:
2000-06
Inhoud:
Gamma-ray curves from surface outcrops together with U-Pb SHRIMP zircon dating are used to redefine the evolution of a Palaeoproterozoic sandy dolostone succession from northern Australia. This case history indicates that gamma-ray logging of surface sections should accompany lithostratigraphic logging or an inadequate interpretation of stratigraphic evolution is a likely outcome. The 1200 m-thick Nathan Group from the McArthur River area had previously been interpreted as a more-or-less continuous package of carbonates deposited in lacustrine and associated shallow-water environments. Now it is seen to comprise the preserved remnants of three truncated, second-order supersequences—the Lawn, Wide and Doom Supersequences—each a few hundred metres thick and each deposited over a time period of a few million years. These supersequences are separated by major stratigraphic breaks each approaching probably 10 million years duration. Each supersequence comprises several third-order sequences which themselves contain higher-order cycles. These were deposited in a series of continental, shoreline, and inner to outer carbonate platform environments. Transgressive, high-energy, fluvial to marginal marine, mixed clastic-carbonate facies dominate most of the sequences. The middle, Wide Supersequence, however, preserves deeper water (mostly sub-storm-wave-base) stromatolitic facies in one sequence, and storm-reworked clastics in another. These are interpreted as condensed intervals deposited around their respective maximum flooding surfaces and are succeeded by regressive facies that probably represent highstand systems tracts. New correlations between these 1615-1575 Ma sandy carbonate successions of the McArthur Basin (Amos, Balbirini and Dungaminnie Formations) and time-equivalent largely clastic successions in the Lawn Hill area (Lawn Hill and Doomadgee Formations), some 400 km to the southeast, are proposed.
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