新近纪-第四纪的后裂陷阶段可分为二个演化阶段，即馆陶组-明二段和明一段-第四系沉积时期。
While, later rifting stage was divided two evolutionary stages which were from Guantao group to Ming-2 member and from Ming-1 member to Quaternary sedimentary period.
新生代裂陷盆地旋回又划分为早期裂陷、强烈裂陷、晚期裂陷和晚第三纪整体坳陷4个阶段。
The latter can be subdivided into 4 stages, including initial rifting, intense rifting, late rifting and Late Tertiary integral downwarping.
金矿容矿地层-岔河组和清水沟组形成于昆阳裂陷槽演化的晚阶段。
The ore- bearing strata, Chahuo Formation and Qingshuigou Formation, were formed in the late stage of the evolution of the Kunyang taphrogeosycline.
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