The Coral Sea has been the host to a variety of large carbonate platforms over the geologic past and presently hosts the world\u27s largest system of coral reefs, the Great Barrier Reef, stretching more then 2,300 km along Australia\u27s northeast coast. The Marion Plateau, which today is the site of 400 m deep hemipelagic sediment drifts, once supported two large carbonate platforms that were precursors to reef growth on the central and southern Great Barrier Reef. Previous work examining the growth phases, drownings and rejuvenation of these platforms is extensive. The purpose of this research is to examine the factors controlling the earliest sedimentation on the margin and how it influenced early development of the carbonate platforms. ...
Overtime, the north Queensland (Australia) and Gulf of Papua (Papua New Guinea) margin has been cons...
The formation of incised valleys on continental shelves is generally attributed to fluvial erosion u...
The formation of incised valleys on continental shelves is generally attributed to fluvial erosion u...
The Coral Sea has been the host to a variety of large carbonate platforms over the geologic past and...
The Coral Sea has been the host to a variety of large carbonate platforms over the geologic past and...
Significant synchronous shifts in the chemistry, mineralogy, grain sizes and color of the sediments ...
Generic models for sediment accumulation predict that fluxes of siliciclastic and neritic carbonate ...
Generic models for sediment accumulation predict that fluxes of siliciclastic and neritic carbonate ...
The continental margin off northeast Australia, comprising the Great Barrier Reef (GBR) platform and...
Generic models for sediment accumulation predict that fluxes of siliciclastic and neritic carbonate ...
The continental margin off northeast Australia, comprising the Great Barrier Reef (GBR) platform and...
The continental margin off northeast Australia, comprising the Great Barrier Reef (GBR) platform and...
I resolved the sedimentary architecture of a shallow water (\u3c 500 m), hemipelagic sediment drift ...
The continental margin off northeast Australia, comprising the Great Barrier Reef (GBR) platform and...
I resolved the sedimentary architecture of a shallow water (\u3c 500 m), hemipelagic sediment drift ...
Overtime, the north Queensland (Australia) and Gulf of Papua (Papua New Guinea) margin has been cons...
The formation of incised valleys on continental shelves is generally attributed to fluvial erosion u...
The formation of incised valleys on continental shelves is generally attributed to fluvial erosion u...
The Coral Sea has been the host to a variety of large carbonate platforms over the geologic past and...
The Coral Sea has been the host to a variety of large carbonate platforms over the geologic past and...
Significant synchronous shifts in the chemistry, mineralogy, grain sizes and color of the sediments ...
Generic models for sediment accumulation predict that fluxes of siliciclastic and neritic carbonate ...
Generic models for sediment accumulation predict that fluxes of siliciclastic and neritic carbonate ...
The continental margin off northeast Australia, comprising the Great Barrier Reef (GBR) platform and...
Generic models for sediment accumulation predict that fluxes of siliciclastic and neritic carbonate ...
The continental margin off northeast Australia, comprising the Great Barrier Reef (GBR) platform and...
The continental margin off northeast Australia, comprising the Great Barrier Reef (GBR) platform and...
I resolved the sedimentary architecture of a shallow water (\u3c 500 m), hemipelagic sediment drift ...
The continental margin off northeast Australia, comprising the Great Barrier Reef (GBR) platform and...
I resolved the sedimentary architecture of a shallow water (\u3c 500 m), hemipelagic sediment drift ...
Overtime, the north Queensland (Australia) and Gulf of Papua (Papua New Guinea) margin has been cons...
The formation of incised valleys on continental shelves is generally attributed to fluvial erosion u...
The formation of incised valleys on continental shelves is generally attributed to fluvial erosion u...