The tectonic fractures mainly formed in the end of Triassic, Cretaceous and Neogene-Early Pleistocene.
构造裂缝主要在三叠纪末、白垩纪末和新近纪末—早更新世末形成。
It is shown that the uplift of the middle Taihang Mountains occurred mainly between the end of Pliocene and Early Pleistocene.
研究同时表明，太行山中段上新世晚期以来的隆升主要发生于上新世末到早更新世时期。
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