Integrating deep-earth and surface processes for frontier-basin exploration. It is well-known that mantle convection has a profound influence on basin evolution, and the next step will be to quantify this relationship and provide the science that will make these concepts applicable to exploration. To do this, we will develop a workflow to link plate-reconstruction software with the mantle convection modelling to link plate motions mantle convection and the history of sedimentation systematically ....Integrating deep-earth and surface processes for frontier-basin exploration. It is well-known that mantle convection has a profound influence on basin evolution, and the next step will be to quantify this relationship and provide the science that will make these concepts applicable to exploration. To do this, we will develop a workflow to link plate-reconstruction software with the mantle convection modelling to link plate motions mantle convection and the history of sedimentation systematically for the first time for frontier basin-scale applications. We will apply these emerging technologies to the evolution of basins in the Arctic borderlands frontier for resource exploration and on the Australian continent.Read moreRead less
Australian Laureate Fellowships - Grant ID: FL0992245
Funder
Australian Research Council
Funding Amount
$3,088,350.00
Summary
The Virtual Geological Observatory: a four dimensional view into the Earth through deep-time data-mining. The Fellowship aims to reveal the underlying processes of plate tectonic cycles, paleogeography, sea-level change and the formation of ore deposits and hydrocarbon resources since the explosion of life during the Cambrian period. Using a mantle convection framework, we will discover how the cyclicity in mid-ocean ridge creation and the subduction dynamics associated with the aggregation and ....The Virtual Geological Observatory: a four dimensional view into the Earth through deep-time data-mining. The Fellowship aims to reveal the underlying processes of plate tectonic cycles, paleogeography, sea-level change and the formation of ore deposits and hydrocarbon resources since the explosion of life during the Cambrian period. Using a mantle convection framework, we will discover how the cyclicity in mid-ocean ridge creation and the subduction dynamics associated with the aggregation and dispersal of Gondwana and Pangea has been driving plate tectonic cycles and cyclicity at the Earth's surface. A Virtual Geological Observatory will transform our understanding of this ancient world by fusing geodata-mining and high-performance computer simulation outputs in the plate-tectonic context.Read moreRead less