Displacement range of Cretaceous MTL and a solution for terrane duplication problem of SW-Japan.

点击翻译按钮获取中文摘要

Displacement rage of MTL was estimated by the provenance analysis using detrital zircon chronology for the Pre-Cretaceous formations in SW-Japan. Zircons from Jurassic accretionary complex in the Inner zone of SW Japan have distinct age cluster at around 1800Ma showing North China origin. While zircons from Outer zone consist mainly of younger generation less than 300Ma. This difference can be traced from western Kyushu to northern Aichi Prefecture. From this, the displacement range of MTL should be larger than 800km.