Plate tectonic forcing leads to changes in the physical conditions that affect the lithosphere.
In response to such changes, notably the local temperature (T) and pressure (P), rocks …

To contribute to our understanding of the mechanisms and pathways of fluid movement
through deeply subducted crust, we investigate high-pressure veins cutting eclogite-facies …

Abstract Activity‐composition (a–x) models have been generated for zirconium‐bearing
haplogranitic silicate melt and garnet from experimental data on zircon dissolution and …

Garnet in high-pressure (HP) to ultrahigh-pressure (UHP) metamorphic rocks in subduction
zone commonly shows considerable zonation in major and trace elements as well as …

Abstract To constrain deep (40–100 km) subduction dynamics, extensive P–T data are
provided on the eclogitic Monviso ophiolite derived from the subducted Liguro‐Piemontese …

Ultra‐high‐pressure eclogites from the Dabie orogen that formed over a range in
temperatures (∼ 600 to> 700° C) have been investigated with combined Lu–Hf and Sm–Nd …

Contiguous continental high-pressure terranes in orogens offer insight into deep recycling
and transformation processes that occur in subduction zones. These remain poorly …

The Monviso meta-ophiolite complex (Northern Italy, Western Alps) represents an almost
intact fragment of Tethyan oceanic lithosphere metamorphosed at~ 80 km depth (~ 2.6 GPa …

We investigated the oceanic-type **ongdian high-pressure eclogites in the western part of
the Dabie orogen with combined U–Pb, Lu–Hf, Sm–Nd and Ar–Ar geochronology. Three …

The kinetics of fluid-driven metamorphic reactions are challenging to study in nature
because of the tendency of metamorphic systems to converge towards chemical equilibrium …