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(jì)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(guó)東部西部均發(fā)育了一系列走滑—拉分性質(zhì)的中新生代盆地，其中有可能發(fā)育一些花狀搆造。
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(rèn)爲(wèi)柴北緣盆地在古近紀(jì)爲(wèi)非對(duì)稱走滑拉分盆地，在新近紀(jì)爲(wèi)擠壓坳陷盆地。

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