Integrating Stress and Strain Data from the North West Shelf, Australia: Implications for Hydrocarbon Seal Integrity. Many exploration wells in the Australian North West Shelf encounter residual columns from which hydrocarbons have leaked due to fault reactivation. Recently there has been a significant increase in our knowledge of contemporary stress (from data such as borehole breakouts)
and strain (from fault reactivation styles) on the North West Shelf.
This project will integrate informati ....Integrating Stress and Strain Data from the North West Shelf, Australia: Implications for Hydrocarbon Seal Integrity. Many exploration wells in the Australian North West Shelf encounter residual columns from which hydrocarbons have leaked due to fault reactivation. Recently there has been a significant increase in our knowledge of contemporary stress (from data such as borehole breakouts)
and strain (from fault reactivation styles) on the North West Shelf.
This project will integrate information on stress and strain in order to investigate whether the current state-of-stress is consistent with
observed reactivation styles, and thus develop predictive models for
fault reactivation and hydrocarbon leakage based on the distribution of
stress and strain.Read moreRead less
The neo- and seismo-tectonics of northwestern Australia. Australia's two largest earthquakes occurred in NW Australia (magnitudes 7 and 7.9 in 1941 and 1906). Onshore and offshore geologic evidence indicates other such events in recent geological history. Our present seismic database records no such events. We propose to document the nature, frequency, intensity, distribution and possible causes of seismicity in NW Australia, through deployment of seismograph arrays. We will test the effects ....The neo- and seismo-tectonics of northwestern Australia. Australia's two largest earthquakes occurred in NW Australia (magnitudes 7 and 7.9 in 1941 and 1906). Onshore and offshore geologic evidence indicates other such events in recent geological history. Our present seismic database records no such events. We propose to document the nature, frequency, intensity, distribution and possible causes of seismicity in NW Australia, through deployment of seismograph arrays. We will test the effects of basement reactivation, determine the crustal structure beneath the cratonic mass, examine onshore and offshore faults, determine local and regional stress orientations and investigate implications for petroleum production in the region, and whether natural resource extraction causes local seismicity.Read moreRead less
Evolution of a two billion year subduction zone: Insights from the integration of microstructure and geochronology. The dynamic evolution of the earth is fundamentally linked to its thermal history. Since, the internal heat production of the earth has changed over time, plate tectonic processes may also have changed over earth history. The manner and timing of this change is highly controversial. We aim to address the nature of tectonic processes 2 billion years ago by studying one of the wor ....Evolution of a two billion year subduction zone: Insights from the integration of microstructure and geochronology. The dynamic evolution of the earth is fundamentally linked to its thermal history. Since, the internal heat production of the earth has changed over time, plate tectonic processes may also have changed over earth history. The manner and timing of this change is highly controversial. We aim to address the nature of tectonic processes 2 billion years ago by studying one of the world's oldest subduction zones (the Usagarian belt in Tanzania). The geometry, kinematics and deformation history of the subduction complex will be integrated with radiometric age dating to quantify the style and rates of ancient tectonic processes.Read moreRead less
Crustal-Scale Fluid Flow in Deep Intracontinental Settings: Conditions, Sources and Deformational Responses. Fluids are important agents of heat and mass transport in the Earth's crust. They play a key role in the mobilisation of metals and as such play a crucial role in the generation of ore deposits. The outcomes of this project will result in a greater understanding of the mechanisms and sources of fluid generation and mobilisation in deep-crustal settings. These outcomes can be related direc ....Crustal-Scale Fluid Flow in Deep Intracontinental Settings: Conditions, Sources and Deformational Responses. Fluids are important agents of heat and mass transport in the Earth's crust. They play a key role in the mobilisation of metals and as such play a crucial role in the generation of ore deposits. The outcomes of this project will result in a greater understanding of the mechanisms and sources of fluid generation and mobilisation in deep-crustal settings. These outcomes can be related directly to the understanding of the controls on the transport and deposition of metals and hence the formation of mineral resources which are vital to maintaining a strong Australian economy.Read moreRead less
Driving Mechanisms of Mountain Building in Accretionary Orogens. Accretionary mountain belts constitute major portions of the Earth's continental crust including the Yilgarn in Western Australia and the area east of Broken Hill constituting a third of the Australian land mass. Understanding the origin of the Permo-Triassic (300-230 Ma) mountain range that lay along the margin of Gondwana from Eastern Australia to South America will provide a new insight into our environment and stimulate interna ....Driving Mechanisms of Mountain Building in Accretionary Orogens. Accretionary mountain belts constitute major portions of the Earth's continental crust including the Yilgarn in Western Australia and the area east of Broken Hill constituting a third of the Australian land mass. Understanding the origin of the Permo-Triassic (300-230 Ma) mountain range that lay along the margin of Gondwana from Eastern Australia to South America will provide a new insight into our environment and stimulate international interest through collaboration amongst researchers around the world. Accretionary orogens are of economic importance as they host the Earth's major orogenic gold deposits and our work has potential to provide a new framework for linking mineralization and deformation events within these important settings.Read moreRead less
Defects and Deformation in Olivine: From Molecules to Mantle. This project establishes the role of hydrogen in controlling olivine deformation, plate tectonics and mantle geodynamics. The unique application of innovative nanoscale simulation, microscale observation and geophysical characterisation ensures that results will have far-reaching impact in the Australian and International Earth Science community. In particular, our results will enable greater understanding of water migration in the m ....Defects and Deformation in Olivine: From Molecules to Mantle. This project establishes the role of hydrogen in controlling olivine deformation, plate tectonics and mantle geodynamics. The unique application of innovative nanoscale simulation, microscale observation and geophysical characterisation ensures that results will have far-reaching impact in the Australian and International Earth Science community. In particular, our results will enable greater understanding of water migration in the mantle, the formation of deep Earth mineral resources and lead to significant improvements in the interpretation of geophysical variations in Earth's lithosphere.Read moreRead less