同生断层也称生长断层、同沉积断层。
The concept of syngenetic fault is known as growth fault or synsedimentary fault.
发育同沉积构造坡折带是断陷盆地的基本特征。
Syndepositional structural slope-break zone is a basic characteristic of rift-subsidence basin.
深水扇系统广布于受同沉积断层控制的古陆架坡折带及其下倾方向。
The deep-water fan systems were spread over paleo shelf-edge and controlled by growth faulting and its down-slope direction.
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