新构造运动出现的地质时期。新构造期，字面上来讲，是指距今最近的构造期。按万天丰(2004)的意见，中国的新构造期从78万年前的中更新世开始，持续至今。
这些发现为研究本区加里东期的大地构造环境和变形特点、扬子板块与华南板块的相互作用提供了新资料。
These findings provide new information for the study of the Caledonian tectonic setting and deformation features in the area and the interaction between the Yangtze and South China plates.
在系统分析北部湾盆地涠西勘查区地震剖面的基础上，认为北部湾盆地涠西勘查区发育两期反转构造即渐新世末期及中新世末期反转构造。
It was indicated that there were two different inversion structures formed in two period based on analysis of seismic profiles in Weixi exploration region of the Beibuwan Basin.
海西-印支期，华南地质构造发展进入新的阶段。
The geologic history of the South China developed into a new stage in the Hercynian - Indochina period.
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