pull-apart
6.The Baise basin is a typical pull-apart basin that w as formed in Tertiary Period.
8.(3) Because of the Ganjiang fault zone influence, Poyang Basin came through complicated tectonic evolution history, which mainly included five developing stages: formation stage of pull-apart basin in Middle Cretaceous, left stripe-slip to rift basin stage in early-middle Later Cretaceous, right stripe-slip & stretch basin stage in late Later Cretaceous, depression stage in Paleogene and rebuilding to residul basin stage in Neogene-Quarternary.
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