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 …

The intraplate rocks of the Dunedin Volcanic Group (DVG) in New Zealand's South Island
erupted in two discrete areas between 25 and 21 Ma before becoming distributed over> …

Alkaline basalts occur widely in intraplate settings and carbonate-bearing mantle sources
such as carbonated peridotites are increasingly regarded to play a key role in their …

To examine how the mantle lithosphere stabilises continents, we present a synthesis of the
mantle beneath Zealandia in the SW Pacific Ocean. Zealandia, Earth's “8th continent” …

Continental intraplate magmas with isotopic affinities similar to HIMU are identified
worldwide. Involvement of an asthenospheric HIMU or HIMU-like source is contested …

New Zealand and the southwest Pacific region have a well-preserved geological record of
Late Cretaceous to Holocene volcanism. Volcanoes and volcanic fields formed in six main …

Systematic variations in the crystal cargo and whole-rock isotopic compositions of mantle-
derived basalts in the intraplate Dunedin Volcano (New Zealand) indicate the influence of a …

Margins resulting from continental breakup are generally classified as volcanic (related to
flood basalt volcanism from a starting plume head) or non-volcanic (caused by tectonic …

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 …

Erebus volcano, Antarctica, is the southernmost active volcano on the globe. Despite its
remoteness and harsh conditions, Erebus volcano provides an unprecedented and unique …