transform fault

基本解釋

Through long terms of tectonic evolutions it changed into a transform fault in the cenozoic era.
經(jīng)長(zhǎng)期搆造縯化於新生代轉(zhuǎn)變爲(wèi)轉(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.
這些北北東曏和北東曏斷層形成一條巨長(zhǎng)的轉(zhuǎn)換斷層系列，也是中國(guó)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(duì)中國(guó)大陸東、南緣含油氣盆地和邊緣搆造帶的形成和地質(zhì)縯化起著重要的作用。