Pliocene

Physical environment since Pliocene and the evolution of fossil man in China

上新世以采的中国自然地理环境和中国古人类的进化

Late Pliocene changes of upper ocean structure in the southern South China Sea

上新世-更新世近海砂层南沙海区晚上新世海水上层结构变化

Paleogeographic change of Yangtze River Delta region since the late Pliocene

长江三角洲地区上新世以来的古地理变化

Pliocene quaternary faulting pattern and left slip propagation tectonics in North China

华北地区上新世至第四纪断裂作用型式与左旋扩展

Changes of organic carbon and paleoproductivity in the southern South China Sea since Middle Pliocene

南海南部中上新世以来沉积有机碳与古生产力变化

Plant Conservation of Western Sichuan PLIOCENE FLORAS OF WESTERN SICHUAN

四川西部高原上新世植物群

Spatial Variation of Grain Size of the Late Pliocene ' Red Clay ', Chinese Loess Plateau

黄土高原晚上新世红粘土粒度的空间变化

Trace elements distribution significance of the Linxia basin from Miocene to Pliocene

临夏盆地中新世至上新世微量元素分布意义上新世-更新世近海砂层

Vegetation succession and climate changing since the Late Pliocene in Tianzhu Region in Beijing

北京天竺晚上新世以来植被演替与气候变迁

Depositional Process in the Huanghe Delta Since Late Pliocene

上新世晚期以来黄河三角洲地区的沉积作用

Progresses in the study of vegetation and climate changes since Pliocene in the Qinghai-Xizang Plateau

青藏高原上新世以来植被与气候研究进展

Some problems concerning correlation of the Pliocene and Miocene Series in Southwest Tarim Basin

塔里木盆地西南地区上、中新统对比中的若干问题

An brief introduction to the global pliocene - pleistocene boundary stratotype section and point

全球上新统-更新统界线层型剖面和点位介绍

The discovery of Eucommia fruit in the Pliocene flora of shanxi , north China

山西上新世杜仲果实的发现

Features of Pliocene strata and lithostratigraphic units on Hainan Island

海南岛上新世地层特征及岩石地层单位

The stomatal data also demonstrate slightly lower Paleo-CO2 concentration in the Late Pliocene than today .

气孔指数还表明，上新世晚期大气CO2浓度较低，略低于目前水平。

Rock type classification of Pliocene Epoch lignite in Jinsuo , Yunnan

云南金所上新世软褐煤的岩石类型分类

The geological age of the present sandstone series is not earlier than the middle-late Pliocene .

因此，含高山栎岩系的地质时代不会早于上新世中晚期。

Research on Four Fossil Plants from the Pliocene in Baoshan of Yunnan and Analysis of Palaeoenvironment

云南保山上新世四种植物化石与古环境分析

The second stage started at Miocene , which was more active period , and finished at Pliocene ;

中新世是喜马拉雅运动的较激烈期，至上新世结束了第二幕。

Their tectonic framework was basically underlain in early Pleistocene or late Pliocene .

它们现在的构造格局基本上是在晚上新世或早更新世奠定的。

Major temperature decrease in the Western Pacific during late Pliocene to early Pleistocene and its paleoclimatic implications

上新世末～更新世初西太平洋变冷事件及其古气候意义

Pliocene Wood Flora from Yuanmou of Yunnan and Taigu of Shanxi , China

云南元谋和山西太谷上新世木化石群研究

Pliocene Rhododendron and Pinus fossil woods of Yunnan Province and Palaeoclimate

云南上新世杜鹃属和松属化石木研究及其古气候意义

Wonambi naracoortensis lived during the Pliocene epoch in Australia .

沃那比蛇生活在上新世时期的澳大利亚。

Variations in upper ocean structure in the South China Sea and the evolution of the East Asian monsoons since late Pliocene

晚上新世以来南海北部上部水体结构变化及东亚季风演化

Eolian origin of the red clay deposits in the Loess Plateau and implications for Pliocene climatic changes

黄土高原红粘土成因及上新世北方干旱化问题

The newest movable of east-west rupture begins the early Pleistocene and Pliocene ;

研究区内东西向断裂最新活动期主要始于早更新世和上新世；

Pliocene environment of Hipparion fauna of middle Himalaya range

喜马拉雅山中段上新世三趾马动物群生活环境的探讨

Shortening napping in the Pliocene epoch and Quaternary period .

上新世&第四纪挤压、推覆阶段。