晚第三纪 meaning in English
neocene
neogene period
Examples
- The phytolith of later pliocene in colorful sand forest of luliang , yunnan
云南陆良彩色沙林晚第三纪地层中的植硅石 - Since late tertiary the neotectonic movement in the region has been being more intense , and the most obvious feature of the neotectonic movement was characterized by large - amplitude block - faulting and strong volcanic activity
晚第三纪以来，本区新构造运动比较强烈，最显著的特徵是断块大幅度升降运动和强烈的火山活动。 - The basin tectonic model : it is intermont basin during late jurassic to early cretaceous , developed into faulted - lacustrine basin in eogene , and evolved into depression in neogene and quaternary
“盆地”构造发育模式为：从晚侏罗世到白垩纪末期发育的山间“盆地”开始、发展到早第三纪断陷湖盆的发育、再演化为晚第三纪及第四纪地陷发育阶段。 - In this paper , we investigated the fruits and seeds in detail from yunnan in the age of miocene and from shanxi in the age of pliocene . 1 . a miocene flora of fruits and seeds is reported from a brown coal mine , named as mangdan , in western yunnan , sw china
本论文首次对我国云南和山西晚第三纪的果实和种子进行专门研究，并根据它们对应的现存最近亲缘植物的分布及生态特征分析和重建了当时当地的古植被、古环境和古气候。 - In a word , the stress field variation since mesozoic can be divided into five periods such as indosinian epoch , early yanshan epoch ( j3 - k1 ) , end of yanshan epoch , eogene , neogene and quaternary , it is mainly affected by the active pattern of tanlu large fault
综合研究认为，本区自中生代以来的应力场变化可分为印支期、早燕山期( j3 - k1 ) 、燕山末期、早第三纪、晚第三纪及第四纪五个阶段，应力场的变化主要受郯庐大断裂活动方式的影响。