transform fault

基本解釋

Through long terms of tectonic evolutions it changed into a transform fault in the cenozoic era.
經長期構造演化于新生代轉變?yōu)檗D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.
這些轉換斷層系統(tǒng)對中國大陸東、南緣含油氣盆地和邊緣構造帶的形成和地質演化起著重要的作用。