Through long terms of tectonic evolutions it changed into a transform fault in the cenozoic era. 經(jīng)長期構(gòu)造演化于新生代轉(zhuǎn)變?yōu)檗D(zhuǎn)換斷層。
These NNE and NE faults become a long transform fault system and formed a boundary between the eastern margin of China Continental Plate and Philippine Sea Plate. 這些北北東向和北東向斷層形成一條巨長的轉(zhuǎn)換斷層系列，也是中國大陸板塊東緣與菲律賓洋塊的一條邊界。
These transform fault series play an important role in the formation and the geological evolution of the Southeastern China continental margin basins and the tectonic-structural zones. 這些轉(zhuǎn)換斷層系統(tǒng)對中國大陸東、南緣含油氣盆地和邊緣構(gòu)造帶的形成和地質(zhì)演化起著重要的作用。