pull-apart basin

基本解释

The fan bodies with their distorted geometry and special sequence assembly provides as a physical parameter of the strike-slip pull apart basins.
走滑拉分盆地中构成特有的歪斜扇体，普遍为向上变粗和变粗又变细的层序。故可以此作为判别古构造性质的物理参数之一。
The USGS describes the geologic setting as “a series of northwest-trending strike-slip (transform) faults that are separated by pull-apart basins.”
USGS把这种地质构造描述为“一系列由裂谷盆地（pull-apart basin）分隔开的西北向走滑断层（转换断层）[见文尾注]”。
Strike-slip or pull-apart sedimentary basins occur in Mesozoic or Cenozoic erathem in East or Mid China, and some flower structures may be discovered in these basins.
我国东部西部均发育了一系列走滑—拉分性质的中新生代盆地，其中有可能发育一些花状构造。