pull-apart basin

基本解釋

The fan bodies with their distorted geometry and special sequence assembly provides as a physical parameter of the strike-slip pull apart basins.
走滑拉分盆地中構成特有的歪斜扇體，普遍為向上變粗和變粗又變細的層序。故可以此作為判別古構造性質的物理參數(shù)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把這種地質構造描述為“一系列由裂谷盆地（pull-apart basin）分隔開的西北向走滑斷層（轉換斷層）[見文尾注]”。
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.
我國東部西部均發(fā)育了一系列走滑—拉分性質的中新生代盆地，其中有可能發(fā)育一些花狀構造。