M. Aoya, P-T-D path of eclogite from the Sambagawa belt deduced from combination ofpetrological and microstructural analyses, J PETROLOGY, 42(7), 2001, pp. 1225-1248
Both structural and petrological data can be wed to constrain the P-T path
of an eclogitic schist unit (the Seba basic schist) in the Sambagawa belt o
f SW Japan. The relationships between these two sets of data are well defin
ed by porphyroblastic and other microstructures. The derived P T path for t
he Seba basic schist has an overall clockwise trajectory with the decompres
sion, or exhumation-related, path taking place under a lower P/T gradient t
han the burial, or subduction-related, path. The clockwise nature of the P
T path is qualitatively, supported by chemical zoning of amphibole coexisti
ng with eclogitic minerals. The significant feature of the P T path is the
presence of two temperature maxima, the first in the eclogite facies, and t
he second in the epidote-amphibolite facies. The existence of two temperatu
re maxima gives a simple explanation for the observation that metamorphic z
onal boundaries postdating the eclogite facies metamorphism cross-cut the d
istribution of the main eclogite bodies in the Sambagawa bell. Estimates of
metamorphic pressure using the jadeite content of clinopyroxene in the Seb
a area demonstrate the existence of a tectonic discontinuity, between the e
clogitic schist and surrounding non-eclogitic schist. Structural studies sh
ow, that although these two units have experienced very different peak meta
morphic conditions, they became juxtaposed during a single ductile deformat
ion affecting both units. This deformation is related to exhumation of the
eclogitic schist and subduction of the non-eclogitic schist, indicating tha
t both were formed during the same subduction event. The presence of a majo
r tectonic boundary between two units with a similar or gain as subducted a
nd accreted material, but contrasting metamorphic histories, can be interpr
eted in terms of nappe tectonics, and the existence of an 'eclogite nappe t
he third nappe of the Sambagawa belt, is proposed.