1.
Plio-Pleistocene paralic sands
上新世-更新世近海砂层
2.
Environmental events and catastrophes from the end of early pleistocene to the early stage of middle pleistocene
早更新世末中更新世早期的环境事件与灾变
3.
SOME QUATERNARY MAMMALIAN FOSSILS FROM NORTHERN ANHWEI
安徽北部更新世哺乳动物化石新产地
4.
Paleoenvironment Evolution in the Okinawa Trough During the Late Pleistocene and Holocene;
冲绳海槽晚更新世——全新世的古环境演化
5.
PLEISTOCENE MAMMALS FROM TUNLIU, SHANXI
山西屯留小常村更新世哺乳动物化石
6.
Analysis of Environment Geology Since Pleistocene in the Source Area of the Huaihe River;
淮河源区更新世以来的地质环境分析
7.
Archaeological Study of Environment and Culture in the Pleistocene Epoch in Henan;
河南更新世环境与文化的考古学观察
8.
Vegetation and climate during the Late Pleistocene in the northern area of Shaanxi
陕西北部地区晚更新世的植被与气候
9.
Late Pleistocene Human Teeth Found in the Huanglong Cave,Yunxi of Hubei Province
湖北郧西黄龙洞更新世晚期人类牙齿
10.
EQUUS QINGYANGENSIS SR.NOV.(PERISSODACTYLA, EQUIDAE) FROM THE EARLY PLEISTOCENE OF QINGYANG,GANSU,CHINA
甘肃庆阳早更新世马属(奇蹄目,马科)一新种
11.
EVOLUTIONARY PROCESS OF THE CLIMATE OF LOP NUR REGION OF XINJIANG SINCE MID-PLEISTOCENE
中更新世以来新疆罗布泊地区气候演化过程
12.
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
13.
The Quantified Estimate of the Temperature from the Late Pliocene to the Early Pleistocene in Nihewan Basin-Based on the Statistics of the Number of Species of Arviclinae;
利用Arvicolinae对泥河湾盆地晚上新世—早更新世古温度定量化研究
14.
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
15.
Tectonic Deformation on Northwestern Margin of Tibetan Plateau during Pliocene-Pleistocene and Uplift of the Tibetan Plateau;
青藏高原西北缘上新世—早更新世构造变形与高原隆升
16.
Adaptive Changes of Hunter-Gatherers during the Late Pleistocene-Early Holocene Transition in China;
中国晚更新世—早全新世过渡期狩猎采集者的适应变迁
17.
Any of various extinct elephantlike mammals of the genus Dinotherium that existed during the Miocene, Pliocene, and Pleistocene epochs.
恐兽一种具有明显类似象的哺乳类动物恐兽，存在于中新世、上新世和更新世时代
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。