1.
LATE PLIOCENE CHANGES OF UPPER OCEAN STRUCTURE IN THE SOUTHERN SOUTH CHINA SEA
南沙海区晚上新世海水上层结构变化
2.
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
3.
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
4.
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
5.
A Quantitative Study on Morphological Variation of Plio-Pleistocene Coccolith Genus Gephyrocapsa from the Northern Region of SCS
晚上新世以来南海北部颗石藻桥石属的定量形态研究
6.
MAMMALIAN FOSSILS FROM LATE PLIOCENE (LOWER MN 16) OF LINGTAI, GANSU PROVINCE
甘肃灵台上新世晚期红粘土中的哺乳动物化石
7.
NOTES ON SOME MAMMALIAN FOSSILS FROM THE UPPER PLEISTOCENE OF WUCHIN,S.KIANGSU
江苏武进县上渎村晚更新世哺乳动物化石
8.
PLANT FOSSILS OF LATE EOCENE FROM WUCHENG,HENAN AND THEIR SIGNIFICANCE IN BOTANY AND PALEOCLIMATOLOGY
河南吴城晚始新世的植物化石及其在植物学、古气候学上的意义
9.
FIRST REPORT OF UPPERMOST LOWER PLIOCENE CALCAREOUS NANNOFOSSIL ASSEMBLAGE AND SEDIMENTARY ENVIRONMENTS FROM NORTHWESTERN HAINAN ISLAND, CHINA
海南岛西北部早上新世晚期颗石藻类组合的发现及沉积环境分析
10.
Study on the Environmental Evolution and the Migration of Ethnic People Since the Late Holocene in Up Reach of Minjiang River;
岷江上游地区晚全新世以来环境变迁与民族迁移
11.
The Shulehe group is of Neogene, in which the Gongxingshan and Getanggou formation are Miocene and Niugetao formation is Pliocene.
疏勒河群时代为晚第三纪,其内的弓形山组、胳塘沟组为中新世,牛胳套组为上新世。
12.
A study on characteristics of the Late Cretaceous-Paleocene structures in Jiuquan Basin
酒泉盆地晚白垩世—古新世构造特征
13.
Plio-Miocene beds
上新世-中新世地层
14.
Plio-Pleistocene paralic sands
上新世-更新世近海砂层
15.
The Baikal rift system was formed due to faulting on the late Cretaceous?Eocene. Epoch planation surface base.
在晚白垩世—始新世夷平面基础上,由于断裂作用形成了贝加尔裂谷系。
16.
Since the beginning of the upper Triassic epoch, the Indian plate upthrusted to the north over the Tethys oceanic crust and led to the closure of the Tethys in Eocene epoch.
晚三迭世开始,印度板块在特提斯洋壳上向北仰冲,并导致特提斯在始新世的关闭。
17.
A NEW BRONTOTHERE FROM LATE MIDDLE EOCENE OF QUFU, SHANDONG
记山东曲阜中始新世晚期─雷兽新属种
18.
A NEW GENUS OF SORICOMORPHA (MAMMALIA) FROMTHE LATH PALEOCENE OF QIANSHAN BASIN, ANHUI PROVINCE
安徽潜山晚古新世??目(哺乳纲)一新属