Pseudosection modelling is rapidly becoming an essential part of a petrologist's toolkit and
often forms the basis of interpreting the tectonothermal evolution of a rock sample, outcrop …

Subduction is a component of plate tectonics, which is widely accepted as having operated
in a manner similar to the present-day back through the Phanerozoic Eon. However …

Eclogite thermobarometry is crucial for constraining the depths and temperatures to which
oceanic and continental crust subduct. However, obtaining the pressure and temperature (P …

The Triassic eclogite-bearing central Qiangtang metamorphic belt (CQMB) in the northern
Tibetan Plateau has been debated whether it is a metamorphic core complex underthrust …

The Sanbagawa belt is a “coherent” oceanic subduction-type metamorphic region
representing a rock package predominantly derived from oceanic crust and accreted at …

The Sumdo complex is a Permian–Triassic eclogitic metamorphic belt in south-east Tibet,
which marks the location of a suture zone that separates the northern and southern Lhasa …

Garnet is the archetypal cubic mineral, occurring in a wide variety of rock types in Earth's
crust and upper mantle. Owing to its prevalence, durability and compositional diversity …

High pressure‐low temperature (HP‐LT) metamorphic rocks structurally beneath the
Tsiknias Ophiolite make up the interior of Tinos Island, Greece, but their relationship with the …

Cooling of the Earth's mantle since the Meso-Archean is predicted by thermal and
petrological models to have induced a secular change in the composition of primary mantle …

In contrast to low‐T eclogites (garnet growth zoning preserved) or high‐T eclogites (garnet
diffusionally homogenized at peak conditions), medium‐temperature eclogites pose …