High-pressure low-temperature (HP–LT) metamorphic rocks provide invaluable constraints
on the evolution of convergent zones. Based on a worldwide compilation of key information …

Although the exhumation of high pressure (HP) and ultrahigh pressure (UHP) rocks is an
integral process in subduction, it is a transient process, likely taking place during the …

High‐pressure metamorphic rocks provide evidence that in subduction zones material can
return from depths of more than 100 km to the surface. The pressure‐temperature paths …

High-P/T metamorphic belts were classified into types A and B according to their protoliths.
The A-type (collision-type) blueschists possess passive-margin protoliths characterized by …

The Franciscan Complex of California records over 150 million years of continuous E-
dipping subduction that terminated with conversion to a dextral transform plate boundary …

The Himalayan range is one of the best documented continent-collisional belts and provides
a natural laboratory for studying subduction processes. High-pressure and ultrahigh …

A broad spectrum of variably altered igneous rocks with a wide range of grain sizes are
compressed and heated over a wide range of pressure-temperature paths in subduction …

Triassic eclogite and blueschist facies rocks occur as a thrust sheet, 25-km long and over 2-
km thick, in an Eocene fold-and-thrust belt in northwest Turkey along the İzmir–Ankara …

Many arc lavas contain material derived from subducted oceanic crust and sediments, but it
remains unresolved whether this distinctive geochemical signature is transferred from the …

The stability and composition of phengitic muscovite was investigated from 5.5–11 GPa, 700–
1150° C in synthesis experiments performed in a multianvil apparatus. Starting materials …