T. Watanabe et al., PRE-MIDDLE SILURIAN GRANITIC MAGMATISM AND ASSOCIATED METAMORPHISM INNORTHERN JAPAN - SHRIMP U-PB ZIRCON CHRONOLOGY, Geological journal, 30(3-4), 1995, pp. 273-280
The results of SHRIMP U-Pb zircon dating are presented for igneous and
metamorphic rocks of enigmatic age in northern Japan. The SHRIMP anal
yses for the Tsubonosawa metamorphic rocks included in the Hikami Gran
ite reveals (1) Ordovician sedimentation of the original rocks, includ
ing Archaean-Proterozoic detrital zircons, and (2) thermal metamorphis
m with partial melting or assimilation followed by intrusion of the Hi
kami Granite at ca. 440 Ma (end of Ordovician). This study allows the
reconstruction of Siluro-Ordovician palaeogeography and mapmatism-asso
ciated metamorphism in East Asia. The SHRIMP results are compared with
those of CHIME (chemical U-Pb total Th isochron method) chronology, w
hich is evaluated as providing significant reconnaissance ages in some
instances.