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 …

New Zealand has a remarkably large number of exhumed mantle occurrences for a small
exposed landmass. Since the last regional syntheses of peridotite (1987) and serpentinite …

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 …

Monogenetic basalts are spatially and temporally unpredictable and are commonly
interpreted to rise extremely rapidly and directly from their mantle source, increasing their …

The basement under the Late Cretaceous unconformity in New Caledonia consists of three
amalgamated terranes. They are all oceanic, arc-related and developed offshore from the …

Deciphering the internal structure and composition of large serpentinite-dominated shear
zones will lead to an improved understanding of the rheology of the lithosphere in a range of …

Volcanoes represent one of the most critical geological settings for hazard modelling due to
their propensity to both unpredictably erupt and collapse, even in times of quiescence …

To investigate the thermal structure of central Te Riu a Māui/Zealandia continent we
estimate the depth to base of magnetic sources (DBMS), using an updated compilation of …

Geophysical data from the monogenetic Auckland volcanic field reveal complex structural
and spatio-temporal relationships at different scales. The volcanic field is coincident with …

Although experiencing some seismicity, the Auckland region is generally considered to be
one of New Zealand's most tectonically stable areas. There is a distinct lack of mapped faults …