泥河湾

泥河湾叠层石样品的ESR与铀系法测年对比

ESR and U-series dating of stromatolite samples from Nihewan basin

caucasicum肢骨，泥河湾标本在性状和尺寸上与其完全一致，进一步证明将这些标本归入E.其中一些肢骨两端项目性别鉴定价值优于长度项目。

On the basis of the limb bones of E. Some measurements at both ends of limb bones have better value for sex determination than measurements of length .

卡盘寿命的延长caucasicum肢骨，泥河湾标本在性状和尺寸上与其完全一致，进一步证明将这些标本归入E。

Lengthening Chuck Life On the basis of the limb bones of E.

河北泥河湾早更新世骨制品的初步观察

Bone artifacts from the early Pleistocene of nihewan , Hebei Province

用多元统计分析方法对泥河湾层的划分与对比

Classification and correlation of Nihewan formation by multivariate statistical analytical method

泥河湾盆地旧石器文化研究新进展

New progress of studies on Paleolithic culture in Nihewan Basin

对泥河湾古猿人葬身处的推测

Inference of Burial Place of Nihewan Ape - man

泥河湾保护区地貌特征与地质灾害

Geomorphic Feature and Geological Calamity in Nihewan Reserve Zone

泥河湾与黄土高原地层对比及其旧石器文化序列

Correlation of the stratigraphy between Nihewan and Loess Plateau and their Paleolithic sequence

河北泥河湾地层化石的电子自旋共振法测年及氨基酸法测年

The ESR and amino-acid dating of fossils from Nihewan beds of Hebei Province

泥河湾古湖湖心区石片的发现

Discovery of a stone flake in the Central District of ancient Nihewan Lake

泥河湾的介形类化石与古环境变迁

Evolution of the fossil population of Ostracodes and change of ancient environment in Nihewan

泥河湾地区第四纪下限问题

The lower boundary of Quaternary in Nihewan area

泥河湾盆地旧石器中晚期石制品原料初步分析

A preliminary study on raw material exploitation in Middle-Upper Paleolithic sites in Nihewan Basin

泥河湾盆地几处旧石器时代文化遗址光释光测年

OSL Dating of the Strata at Paleolithic Sites in the Nihewan Basin , China

对泥河湾地层的认识与划分

Subdivision and recognition of the Nihewan strata

泥河湾盆地沉积物磁化率及粒度参数对沉积环境的响应

The Sediment Susceptibility and Grain-size Profile Respond to Change of Depositional Environment in Nihewan Basin

其中，在0.96～0.95Ma间，古泥河湾湖具有较高的温度、盐度特征。

Therein , within 0.96 0.95 Ma , Nihewan Lake had considerably high temperature and salinity .

丙烯酸树脂非水分散体加固剂在泥河湾古象足痕迹提取中的应用

Application of acrylic non-aqueous dispersion as consolidation for ancient elephant foot-prints discovered at Nihewan Paleolithic site

河北阳原盆地泥河湾组有孔虫来源的探讨

Approach on Sources of Foraminifera and Environment of Deposition in Nihewan Group of Yangyuan Basin , Hebei Province

泥河湾盆地的水下黄土堆积及其古气候意义

Underwater loess and paleoclimate

孙殿卿教授等后来在河北省泥河湾划分出六个冰期与五个间冰期。

Five glacial stages and four interglacial stages were divided by Professor Li Chengshan from the northwestern Sichuan plateau .

铁磁/反铁磁双层膜中的磁化性质与界面微结构泥河湾盆地层序地层学与磁性地层学综合研究

Computer Simulation of Magnetic Properties of Composite Bilayer Magnetic Films Interfacial microstructure dependence of magnetization feature in ferromagnetic / antiferromagnetic bilayers

等温剩磁获得曲线的累积对数高斯模型在泥河湾盆地磁组分识别中的运用

Identification of remanence carrying minerals of Nihewan samples , using the modeling of isothermal remanent magnetization acquisition curves by cumulative log Gaussian functions

记录中国北方晚新生代以来地球演化、生物进化与古人类活动的泥河湾层，是珍贵的地质遗迹。

According to the records of early human activities , Nihewan strata is an invaluable geological relic that has undergone the evolution of the earth and creations since the later Cenozoic Era .

应用古地磁学原理，分析了中国北方第四纪黄土、泥河湾盆地、黄海陆架磁性地层记录的古地磁极倒转与气候变化之间的关系。

This paper analyzed the relationship between paleomagnetic polarity reverse and climatic change recoded by magnetostratigraphy of loess , Nihewan Basin and Yellow Sea shelf in Northern China during Quaternary by paleomagnetism .

剖面下部河流相含砾中粗砂层至中部河流相砂砾层之间的湖相灰绿、灰黄色粘土质粉砂和粉砂质粘土层称泥河湾组；

The lacustrine grayish green and grayish yellow clayey silt and silty clay beds between fluvial gravel-bearing medium-coarse sand beds in the lower part of the section and fluvial sand and gravel beds in the middle part are called the Nihewan Formation ;

泥河湾盆地旧石器文化异常丰富，在约1800平方公里范围内新发现各时期的旧石器文化遗址或地点三十余处，这些发现为该盆地旧石器文化研究提供了大批的科学资料。

The paleolithic cultural sites are very plentiful in the Nihewan Basin , More than thirty sites of various period have been found recently in the Basin . These discovery provided a large quantity of scientific information for the research of paleolithic culture .

研究结果表明：在0.97～0.94Ma间，古泥河湾湖为一陆相湖泊，湖水的温度、盐度变化趋势相吻合，均呈低高低的演化特征，可能对应着盆地水体的扩展退缩扩展变化。

The results revealed that within 0.97 0.94 Ma , Nihewan was a continental lake , the variation tendency of temperature and salinity is consistent from low high low . Maybe , they are corresponding to a tendency of expansion retreat expansion of the water body .