Funder: Geoscience AustraliaFunder: Shell Global, Shell Exploration and Production Company; Id: http://dx.doi.org/10.13039/100011092Abstract: Spatio‐temporal changes of upper mantle structure play a significant role in generating and maintaining surface topography. Although geophysical models of upper mantle structure have become increasingly refined, there is a paucity of geologic constraints with respect to its present‐day state and temporal evolution. Cenozoic intraplate volcanic rocks that crop out across eastern Australia provide a significant opportunity to quantify mantle conditions at the time of emplacement and to independently validate geophysical estimates. This volcanic activity is divided into two categories: age‐progressive pr...
To discern temperature and compositional variations of the Australian upper mantle, we apply an inte...
To discern temperature and compositional variations of the Australian upper mantle, we apply an inte...
To discern temperature and compositional variations of the Australian upper mantle, we apply an inte...
Plain Language Summary Earth's convecting mantle lies between the tectonic plates and the core. Thi...
Density variations and viscous flow within the convecting mantle generate deflections of the Earth’s...
Eastern Australia includes Cenozoic mafic volcanic provinces that are commonly divided into age-prog...
Mantle convection is important in understanding the heat flow and thermal structure of the continent...
The >1090 to <1040Ma Giles Event added extraordinary volumes of mantle derived magma to the cr...
Many intraplate volcanic provinces do not appear to originate from plate-boundary processes or upwel...
Mantle convection is important in understanding the heat flow and thermal structure of the continent...
[1] Despite its importance, the spatial and temporal pattern of dynamic topography generated by mant...
Despite its importance, the temporal and spatial evolution of continental dynamic topography is poor...
Basalt fields and central volcanoes form a curved south-migrating trace through NW New South Wales. ...
Many intraplate volcanic provinces do not appear to originate from plate-boundary processes or upwel...
Copyright 2009 by the American Geophysical Union.[1] Tectonic models for the latest Paleoproterozoic...
To discern temperature and compositional variations of the Australian upper mantle, we apply an inte...
To discern temperature and compositional variations of the Australian upper mantle, we apply an inte...
To discern temperature and compositional variations of the Australian upper mantle, we apply an inte...
Plain Language Summary Earth's convecting mantle lies between the tectonic plates and the core. Thi...
Density variations and viscous flow within the convecting mantle generate deflections of the Earth’s...
Eastern Australia includes Cenozoic mafic volcanic provinces that are commonly divided into age-prog...
Mantle convection is important in understanding the heat flow and thermal structure of the continent...
The >1090 to <1040Ma Giles Event added extraordinary volumes of mantle derived magma to the cr...
Many intraplate volcanic provinces do not appear to originate from plate-boundary processes or upwel...
Mantle convection is important in understanding the heat flow and thermal structure of the continent...
[1] Despite its importance, the spatial and temporal pattern of dynamic topography generated by mant...
Despite its importance, the temporal and spatial evolution of continental dynamic topography is poor...
Basalt fields and central volcanoes form a curved south-migrating trace through NW New South Wales. ...
Many intraplate volcanic provinces do not appear to originate from plate-boundary processes or upwel...
Copyright 2009 by the American Geophysical Union.[1] Tectonic models for the latest Paleoproterozoic...
To discern temperature and compositional variations of the Australian upper mantle, we apply an inte...
To discern temperature and compositional variations of the Australian upper mantle, we apply an inte...
To discern temperature and compositional variations of the Australian upper mantle, we apply an inte...