pull-apart

基本解释

The Baise basin is a typical pull-apart basin that was formed in Tertiary Period.
百色盆地是一典型的第三纪走滑拉分盆地。
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。
Therefore, the authors consider that the basin was an asymmetrical strike-slip pull-apart basin in the Palaeogene but becomes a compressive depression basin in Neocene.
因此，认为柴北缘盆地在古近纪为非对称走滑拉分盆地，在新近纪为挤压坳陷盆地。

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