Restraining-and releasing bends with similar morphology and structure have been
described by many previous studies of strike-slip faults in a variety of active and ancient …

Progressive vapour‐absent partial melting of a closed rock system increases melt pressure
due to an expansion in the volume of the mineral plus melt assemblage. For a locally closed …

It is generally accepted that the subduction polarity reversal (SPR) results from the strong
collision of two plates. Yet, the SPR of the Solomon Back‐arc Basin is started in the “soft …

We present measurements of hydrogen and oxygen isotopes in MORB glasses from
Macquarie Island (SW. Pacific Ocean) coupled with determination of bulk H2O content by …

Two geochemically and temporally distinct components of the Mesozoic Zealandia
Cordilleran arc indicate a shift from low to high Sr/Y whole rock ratios at c. 130 Ma. Recent …

Magnesian basaltic glasses from the Miocene Macquarie Island ophiolite (SW Pacific) are
used for understanding the effects of progressive partial melting of the mantle peridotite, and …

Water is critical in the evolution of the mantle due to its strong influence on the
physicochemical properties of mantle rocks. Mid‐ocean ridge basalts (MORBs) are …

Identification of melt–rock interaction during melt flux through crustal rocks is limited to field
relationships and microstructural evidence, with little consideration given to characterising …

The timing and mode of uplift of the Troodos ophiolite are constrained by low‐temperature
thermochronology combined with geomorphic analysis. Zircon (U‐Th)/He and apatite fission …

The foraging strategies of king penguins from Heard and Macquarie islands were compared
using satellite telemetry, time-depth recorders and diet samples. Trip durations were …