pull-apart

基本解釋

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紀走滑拉分盆地。
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。
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，認為柴北緣盆地在古近紀為非對稱走滑拉分盆地，在新近紀為擠壓坳陷盆地。

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