上新世

云南金所上新世软褐煤的岩石类型分类

Rock type classification of Pliocene Epoch lignite in Jinsuo , Yunnan

上新世&第四纪挤压、推覆阶段。

Shortening napping in the Pliocene epoch and Quaternary period .

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。

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

上新世是本区最主要的非烃类气体的成藏期。在岩浆活动以前形成并与气源断裂直接连通的构造为CO2气聚集的有利圈闭。

The structures that formed prior to magmatic activities and are connected with gas_source faults may be traps favorable to CO 2 accumulation .

吐哈盆地层间氧化还原带型铀矿化前锋处于相对不稳定状态，在上新世以后成矿物质U仍具有迁移活动发生；

The front of the interlayer oxidation zone type mineralization in Turpan-Hami basin is in a relatively unstable condition , and the ore-forming material U still migrated after Pliocene .

柯坪东西向断裂系统的主要活动期是上新世（N2）以后。

It is pointed out that the E-W fracture system in Kalpin area was active mainly after Pliocene ( N 2 ) .

层序IV，在陆坡和岛弧地区都有分布，但是在海槽盆地内部区域缺失该层序，为上新世沉积物。

We found that sequence IV , which is Pliocene sediments , only exists in the slope and island arc slope and not distributes in the trough basin .

断块运动受统一应力场支配，早期（渐新世上新世）主压应力方向为NESW，晚期（上新世末第四纪）则转为NWSE。

Fault-block movement is controlled by the unified regional stress field . The principle compression stress direction was NE SW during the early neotectonic stage ( E_3 N_2 ) , while in the late stage ( the end of N_2 Q ) it 's become to NW SE .

沉积于中中新世到上新世的浊积砂体是第三纪Niigata弧后盆地的主要油气储层之一，该盆地是日本列岛最富产石油的盆地。

Many turbidite sandstone bodies , deposited during the Middle Miocene to Pliocene , are distributed and form one of major reservoirs for oil and gas in the Tertiary Niigata backarc sedimentary basin , the most productive oil basin in the Japanese Islands .

前陆盆地中分布最广泛的为Siwalik群，它占据了次喜马拉雅带的绝大部分，时代主要为中新世-上新世早期。

It outcrops in Potwar plateau ( Pakistan ) and was deposited from middle-Eocene to earlier-Miocene . The Siwalik Group ( Miocene to Pliocene ) has the widest distribution and covers most part of Sub-Himalaya zone .

帕米尔&西昆仑北麓前陆褶皱冲断带的主要构造变形时间始于上新世早期（距今约4.6Ma），断层、褶皱的变形时代由山前向盆地逐步变新，变形强度由山脉向塔里木盆地逐步减弱。

The main tectonic deformation in the Pamir Western Kunlun foreland fold and thrust belt started in Early Pliocene ( about 4.6 Ma ago ), and migrated gradually from the orogen to the foreland basin , with the faulting and folding becoming younger and weakened in the basin .

长江三角洲地区上新世以来的古地理变化

Paleogeographic change of Yangtze River Delta region since the late Pliocene

云南上新世杜鹃属和松属化石木研究及其古气候意义

Pliocene Rhododendron and Pinus fossil woods of Yunnan Province and Palaeoclimate

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

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

上新世-更新世近海砂层海砂在福建地区混凝土中的应用前景

The Application Perspective of Sea Sand in Concrete of Fujian

华北地区上新世至第四纪断裂作用型式与左旋扩展

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

四川西部高原上新世植物群

Plant Conservation of Western Sichuan PLIOCENE FLORAS OF WESTERN SICHUAN

海南岛上新世地层特征及岩石地层单位

Features of Pliocene strata and lithostratigraphic units on Hainan Island

中新世和上新世的旧大陆人科的一属。

Genus of Old World hominoids ; Miocene and Pliocene .

沃那比蛇生活在上新世时期的澳大利亚。

Wonambi naracoortensis lived during the Pliocene epoch in Australia .

上新世以采的中国自然地理环境和中国古人类的进化

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

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；

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

生活在上新世至更新世时期的巨型陆栖类哺乳动物，外形似树懒，现已灭绝。

Gigantic extinct terrestrial sloth-like mammal of the Pliocene and Pleistocene in America .

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

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

乳齿象不是来自上新世吗？

Isn 't the mastodon from the Pliocene epic ?

上新世-第四纪区域沉降阶段，东西向断层再次活动。

Regional subsidence stage from Pliocene to Quaternary , the EW trending reactivated .

喜马拉雅山中段上新世三趾马动物群生活环境的探讨

Pliocene environment of Hipparion fauna of middle Himalaya range

云南元谋和山西太谷上新世木化石群研究

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

上新世晚期以来黄河三角洲地区的沉积作用

Depositional Process in the Huanghe Delta Since Late Pliocene

山西上新世榆属炭屑的发现及其生态学意义

Pliocene charcoal woods of Ulmus from Taigu basin , Shanxi and their ecological implication