Small-scale volcanic systems are the most widespread type of volcanism on Earth and occur
in all of the main tectonic settings. Most commonly, these systems erupt basaltic magmas …

ABSTRACT Auckland Volcanic Field (AVF) is a basaltic intraplate volcanic field in North
Island, New Zealand, upon which> 1.6 million people live. Seismic velocity tomography and …

Many intraplate volcanic provinces do not appear to originate from plate-boundary
processes or upwelling mantle plumes. Edge-driven convection (EDC), where a small-scale …

Most of Earth's volcanism occurs at plate boundaries, in association with subduction or
rifting. A few high-volume volcanic fields are observed both at plate boundaries and within …

Several of Earth's intraplate volcanic provinces are hard to reconcile with the mantle plume
hypothesis. Instead, they exhibit characteristics that are more compatible with shallower …

High-resolution sampling in monogenetic fields has the potential to reveal fine-scale
heterogeneity of the mantle, a feature that may be overwhelmed by larger fluxes of magma …

We present a new S-wave velocity tomographic model of the upper mantle beneath the
Australian Plate and its boundaries that we call Aus22. It includes azimuthal anisotropy and …

The Australian continent is actively deforming in response to far-field stresses generated by
plate boundary interactions and buoyancy forces associated with mantle dynamics. On the …

Despite its importance, the temporal and spatial evolution of continental dynamic
topography is poorly known. Australia's isolation from active plate boundaries and its rapid …

Small scale basaltic magmatic systems occur in all of the major tectonic environments of
planet Earth and are characteristically expressed at the Earth's surface as fields of small …