The use of outcrop analogues to characterise large-scale deepwater sedimentary architecture. Deepwater turbidite sedimentary systems are one of the modern frontiers in petroleum exploration, with many major discoveries expected from around the world in the next 25 years. Technological advances in the drilling and production of the deepwater hydrocarbons now enable the exploration and exploitation in this realm. However, the geometry, internal architecture and spatial variations of deepwater sand ....The use of outcrop analogues to characterise large-scale deepwater sedimentary architecture. Deepwater turbidite sedimentary systems are one of the modern frontiers in petroleum exploration, with many major discoveries expected from around the world in the next 25 years. Technological advances in the drilling and production of the deepwater hydrocarbons now enable the exploration and exploitation in this realm. However, the geometry, internal architecture and spatial variations of deepwater sandbodies are still poorly understood. By using state-of-the-art outcrop, modern submarine fan and petroleum exploration data, this research project will improve the understanding of the reservoir geometry and internal architecture of deepwater sandbodies. The results will aid in the exploration and development of hydrocarbons in deepwater sedimentary systems.Read moreRead less
Constraining the snowball earth: timing and duration of neoproterozoic glaciations using precise Re-Os geochronology. This project aims to investigate the onset and duration of major global glacial events during the period of Earth history when metazoan life first appeared. Understanding such processes will enable insights into both the rate and nature of evolutionary processes, and place constraints of ancient and modern climate models. This will be achieved by establishing a facility to obtain ....Constraining the snowball earth: timing and duration of neoproterozoic glaciations using precise Re-Os geochronology. This project aims to investigate the onset and duration of major global glacial events during the period of Earth history when metazoan life first appeared. Understanding such processes will enable insights into both the rate and nature of evolutionary processes, and place constraints of ancient and modern climate models. This will be achieved by establishing a facility to obtain precise Re-Os isotope age data from sediments at Adelaide University (only the second such in the world), and studying sedimentary rocks preserved in the Centralian Superbasin. A basis for global stratigraphic correlation will also result from the intended program of work.Read moreRead less
Longshore Sediment Supply to the Deep Ocean. The current model to supply sand to deep water off continental margins is that provided by rivers operating at low sea level. We propose an alternative model in which sand is provided by longshore transport to deep water at high sea level north of Fraser Island, SE Queensland. Here we will test the validity of our new model by site studies of sea bottom morphology, composition and dynamics. If the model proves true, we will have: 1) generated an entir ....Longshore Sediment Supply to the Deep Ocean. The current model to supply sand to deep water off continental margins is that provided by rivers operating at low sea level. We propose an alternative model in which sand is provided by longshore transport to deep water at high sea level north of Fraser Island, SE Queensland. Here we will test the validity of our new model by site studies of sea bottom morphology, composition and dynamics. If the model proves true, we will have: 1) generated an entirely new exploration model for deepwater hydrocarbons, 2) provided new expertise and seabed maps for generating a superior marine naval defence capability.Read moreRead less
The stratigraphic architecture of continental margins (MARGINS). The project seeks to increase our understanding of how continental margins develop. Emphasis is given to studying the controls exerted on sedimentation by sea-level change, climate cycling, ocean front location, current-deposition and tectonics, using the southwest Pacific (temperate eastern NZ) as the prime fieldwork area. Sediment being transported across continental margins passes through a number of energy fences (e.g. piedmont ....The stratigraphic architecture of continental margins (MARGINS). The project seeks to increase our understanding of how continental margins develop. Emphasis is given to studying the controls exerted on sedimentation by sea-level change, climate cycling, ocean front location, current-deposition and tectonics, using the southwest Pacific (temperate eastern NZ) as the prime fieldwork area. Sediment being transported across continental margins passes through a number of energy fences (e.g. piedmont, shoreline, wave-base, storm-zone, shelf-edge), which together modulate sediment transport and deposition. These fences differ in their relative positions, magnitudes and effects on different margins. The research will combine onland and offshore studies, builds on data collected during ODP Leg 181, and is integrated with the international MARGINS "source to sink" program.Read moreRead less