The Initiation and 3D Evolution of Instabilities in the Deep Continental Lithosphere. This project is part of a new international initiative in the Geodynamics of the Australian Plate bringing together studies of the active tectonics of the boundary regions of our plate and the ancient analogues of these processes which are locked into the stable interior of the Australian continent. The proposed research is a good fit to the Identification and Extraction of Deep Earth Resources priority goal. D ....The Initiation and 3D Evolution of Instabilities in the Deep Continental Lithosphere. This project is part of a new international initiative in the Geodynamics of the Australian Plate bringing together studies of the active tectonics of the boundary regions of our plate and the ancient analogues of these processes which are locked into the stable interior of the Australian continent. The proposed research is a good fit to the Identification and Extraction of Deep Earth Resources priority goal. Detachment of the lithosphere is associated with fertile mantle being emplaced at shallow depth below the crust; an important precursory event for mineralization. The project builds upon AuScope (NCRIS 5.13) to create infrastructure for a new, smart resource exploration and extraction industry based on modelling and simulation.Read moreRead less
A new rheological model for Australia to improve seismic hazard estimates and study the region's recent tectonic history and landform evolution. Australia is currently being squeezed between three active mountain belts, the Himalayas, the Papua New Guinea Highlands and the Southern Alps in New Zealand. We propose to integrate a large number of geological and geophysical databases that have been collected over the past few decades to develop a three-dimensional rheological model of the Australian ....A new rheological model for Australia to improve seismic hazard estimates and study the region's recent tectonic history and landform evolution. Australia is currently being squeezed between three active mountain belts, the Himalayas, the Papua New Guinea Highlands and the Southern Alps in New Zealand. We propose to integrate a large number of geological and geophysical databases that have been collected over the past few decades to develop a three-dimensional rheological model of the Australian continent, that is a model that predicts where and how Australia is deforming today. Combined with new, targeted field work, this model will be used to predict where earthquakes are likely to take place but also to study how our old continent is affected by these active mountain belts to create the present-day landscapes in which we live.Read moreRead less