Eclogites are witnesses of geodynamic processes that are commonly related to subduction
of oceanic crust. Information on the part of these processes that refers to the burial of this …

U-Pb geochronology by isotope dilution–thermal ionization mass spectrometry (ID-TIMS)
has the potential to be the most precise and accurate of the deep time chronometers …

Empirical studies of zircon in migmatites document features compatible with growth during
heating at suprasolidus conditions. However, numerical modelling of zircon behaviour …

Mineral inclusions are ubiquitous in metamorphic rocks and elastic models for host‐
inclusion pairs have become frequently used tools for investigating pressure–temperature (P …

Dehydration reactions within subducted oceanic crust are important for fluid‐mediated
element transfer within the subducting plate and potentially to the mantle wedge. The effects …

Abstract The Changning–Menglian orogenic belt (CMOB) in the southeastern Tibetan
Plateau is an important link between the Longmu Co–Shuanghu suture (LCSS) in the …

The compositional range of∼ 2,000 marine sediments and∼ 19,000 oceanic igneous rocks
is encapsulated by a set of 12 sedimentary and 10 mafic rock compositions, allowing …

The Shuanghe garnet‐bearing paragneiss from the Dabie ultra‐high–pressure (UHP)
orogen occurs as an interlayer within partially retrogressed eclogite. A first UHP …

Abstract In the Monte Duria area (Adula-Cima Lunga unit, Central Alps, N Italy) garnet
peridotites occur in direct contact with migmatised orthogneiss (Mt. Duria) and eclogites …

Mineral compositions and textures of Late Miocene coesite eclogite from Tomagabuna
Island were investigated to constrain P–T conditions during UHP metamorphism and …