Pliocene
- n.上新世
- adj.上新世的
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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
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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
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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
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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
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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
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Plant Conservation of Western Sichuan PLIOCENE FLORAS OF WESTERN SICHUAN
四川西部高原上新世植物群
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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
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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
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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
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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
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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
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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
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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
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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
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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
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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。
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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
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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。
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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
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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。
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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。
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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
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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
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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
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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。
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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
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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
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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;
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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
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Shortening napping in the Pliocene epoch and Quaternary period .
上新世&第四纪挤压、推覆阶段。