1.
Study on species niche of Schima superba and Pinus massoniana artificial forest shrub layer
木荷马尾松林更新层种群生态位分析
2.
Plio-Pleistocene paralic sands
上新世-更新世近海砂层
3.
Go upstairs further with our best efforts──New year message
努力登攀 更上一层楼─—新春寄语
4.
Changing View of Development and Doing Environmental Protection Work of Grass Roots Well;
更新发展观念 做好基层环保工作
5.
Developing And Manufacturing More And Better Double Deck Passenger Cars Congratulations on the Tenth Anniversary of Operation of the New Type of Double Deck Passenger Cars;
研制开发更多更好的双层客车——祝贺新型双层客车运营10周年
6.
Lithostratigraphy,Biostratigraphy and Climatic Stratigraphy in the North China Plain since Late Pleistocene
华北平原晚更新世以来岩石地层、生物地层及气候地层
7.
Sequence Stratigraphy of Pliocene-Eopleistocene Epoch and Its Paleoenvironmental Significance in Zanda Basin, Tibet;
西藏札达盆地上新世—早更新世层序地层学及其古环境意义
8.
While many old problems still remain to be solved, many new ones are emerging.
很多旧问题需要继续解决，新问题更是层出不穷。
9.
This is an unalterable law of nature, and old leaders have to be continually replaced by new ones.
自然规律是不可改变的，领导层更新也是不断的。
10.
Early Man and Pleistocene Stratigraphy in Southern and Eastern Asia by Hallam L, Movins Jr.
亚洲东南化石人及更新统地层莫维士著
11.
Research of Transformation for Shenzhen s Low Income Social Stratum s Daily Active-space;
深圳城市低收入阶层生活空间更新研究
12.
Magnetostratigraphy Study of the Pleistocene Nanzhai Section (Xiangfen, Shanxi);
山西襄汾更新世南寨剖面的磁性地层学研究
13.
An Inquiry into Annual Updating of NFI Data under Stratified Sampling
分层抽样下的森林资源清查数据年度更新探讨
14.
The origin of the Pleistocene gravel in western Sichuan depression
川西凹陷地区更新统砾石层沉积成因探讨
15.
Groundwater Renewal and Characteristics in the Deep Confined Aquifer in North China Plain
华北平原深层地下水的更新与资源属性
16.
Chemical Element Distribution and Palaeoclimate in Late Pleistocene-Holocene Strata in East Gonghe Basin
青海共和盆地东部晚更新世——全新世地层中元素分布与古气候
17.
THE DISCOVERY OF THE EOPLEISTOCENE GLACIAL DEPOSIT IN XINJIANG WEST KUNLUN TIANWENTAI AREA AND ITS SIGNIFICANCE
新疆西昆仑天文点一带发现早更新世冰碛层及其意义
18.
The eastern Yantai-Weihai segment is a mid Pleistocene segment on which no late Pleistocene offset has been found.
东段烟台－威海段为中更新世活动段，没有发现晚更新世地层错断现象。