晚新生代地壳构造运动 late Cenozoic crustal tectonism
酒西盆地旱峡和红柳峡等地有基性火山岩产出，它们曾一度被认为是新生代构造运动的产物。
The volcanic rocks from Hanxia and Hongliuxia in Jiuxi basin are considered to be resulted from Cenozoic tectonic events.
位于青藏高原北缘的酒西盆地晚新生代沉积比较敏感和全面记录了高原北部的构造运动和隆升过程。
The sediments of the late Cenozoic in the Jiuxi basin, located in the northern margin of the Tibetan plateau, have sensitively and completely recorded the uplifting process of northern plateau.
本文对晚新生代贵州喀斯特地貌演进的三大控制因素 ，即地质基础、新构造运动及挽近气候波动进行了分析论证。
In this paper, three determined factors influencing on the evolution of karst geomorphology of upper Cenozoic in Guizhou, e.
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