Maximum shear stress along an active deformation zone marking the subduction plate
interface is important for understanding earthquake phenomena and is an important input …

In the Iratsu and the quartz-bearing eclogite bodies of the Sanbagawa high-pressure type
metamorphic belt, southwest Japan, zircon U–Pb dating and trace-element analysis of the …

Large parts of the shallow mantle wedge are thought to be hydrated due to release of fluids
from the subducting slab and serpentinization of the overlying mantle rocks. If …

The Sanbagawa metamorphic belt of southwest Japan is one of the type localities of
subduction‐related high‐P metamorphism. However, variable pressure–temperature (P–T) …

The relationships between the relative B–Li–Cl compositions of deep fluids and their
entrapment depth were investigated by means of geochemical studies of fluid inclusions in …

The geochemical evolution of metamorphic rocks during subduction‐related metamorphism
is described on the basis of multivariate statistical analyses. The studied data set comprises …

Abstract The Western Iratsu body of the Sanbagawa belt (SW Japan) is a mafic–ultramafic
complex that underwent an initial metamorphism in the amphibolite facies and a subsequent …

Quantitative analyses of garnet-bearing epidote amphibolite (hereafter garnet amphibolite)
from the Funaokayama unit, western Kii Peninsula of the Sanbagawa belt reveal a …

Detailed morphological studies including phase-volume estimation were performed on a
natural fluid inclusion in an eclogite-facies rock collected from the Sanbagawa metamorphic …

Here we first report the in situ U–Pb dating of metamorphic grossular garnet (Grs) with
distinction between internal zonation textures. The studied Grs occurs in an eclogite–facies …