Jp. Encarnacion et al., HIGH-PRESSURE AND TEMPERATURE SUBOPHIOLITIC KYANITE-GARNET AMPHIBOLITES GENERATED DURING INITIATION OF MID-TERTIARY SUBDUCTION, PALAWAN, PHILIPPINES, Journal of Petrology, 36(6), 1995, pp. 1481-1503
Metamorphic rocks exposed near the base of a pre-middle Eocene ophioli
te in central Palawan, Philippines preserve a record of the P-T-t cond
itions under which the ophiolite was detached and emplaced onto the ri
fted southeast margin of China. Garnet amphibolites in contact with ma
ntle harzburgite preserve peak metamorphic temperatures of 700-760 deg
rees C and minimum pressures of 9 kbar, consistent with the presence o
f kyanite. Garnet grains which preserve strong prograde zoning (Pyp(11
) in cores to Pyp(43) in rims) contain inclusion assemblages that cons
train pressures above 5-6 kbar at 400-500 degrees C. This represents a
n early prograde clockwise Path consistent with underthrusting. Two am
phibolite samples yield hornblende Ar-39/Ar-40-Ar-36/Ar-40 isochron ag
es of 34.0+/-0.6 Ma (2 sigma) (early Oligocene), which are indistingui
shable from a 34.3+/-0.2 Ma isochron age of muscovite from a kyanite -
chlorite - muscovite schist that is interlayered with the amphibolite
s. The high pressures (equivalent to a depth of >30 km in oceanic lith
osphere) and temperatures, and the age difference between ophiolite cr
ystallization and metamorphism of the sole, are incompatible with the
rocks having formed in a mature subduction zone or oceanic spreading c
enter. Instead, the timing, P-T conditions, and regional geology sugge
st metamorphism in a nascent subduction zone. Rapid cooling and exhuma
tion of the metamorphic rocks followed peak metamorphic conditions in
the earliest Oligocene, perhaps by the rapid thickening of the accreti
onary complex that is preserved beneath the ophiolite. The amphibolite
s formed during the inception of southward subduction within proto-Sou
th China Sea oceanic lithosphere south of the Eurasian margin. This le
d to the formation of an arc-trench system that accommodated extension
along southeast China and the opening of the South China Sea.