1.
DISCOVERY OF PROTITAN (PERISSODACTYLA, BROTOTHERIIDAE) FROM LATE EOCENE TUKHUM BEDS, NEI MONGOL
内蒙古晚始新世土克木层发现之原雷兽
2.
LATE EOCENE MAMMALIAN FAUNAS OF HONAN AND SHANSI WITH NOTES ON SOME VERTEBRATE FOSSILS COLLECTED THEREFROM
河南、山西晚始新世哺乳类化石地点与化石层位
3.
LATE EOCENE MAMMALS FROM PINGCHANGGUAN BASIN, HENAN
河南信阳平昌关盆地晚始新世哺乳动物化石
4.
THE FIRST DISCOVERY OF LATE EOCENE LOCALITY OF MAMMALIAN FAUNA IN EAST CHINA
山东首次发现晚始新世哺乳动物化石地点
5.
LATE EOCENE AND OLIGOCENE CHAROPHYTES FROM THE DONGPU AREA, HENAN AND THEIR PALAEOENVIRONMENTAL SIGNIFICANCE
河南东濮地区晚始新世至渐新世轮藻植物群及其古环境探讨
6.
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
7.
IRDIN MANHA UPPER EOCENE AND ITS MAMMALIAN FAUNA AT HUHEBOLHE CLIFF IN CENTRAL INNER MONGOLIA
内蒙古呼和勃尔和陡坎晚始新世伊尔丁曼哈层及其哺乳动物群
8.
LATE EOCENE QUATERNARY RADIOLARIA FROM THE NORTHEAST OF THE PHILIPPINE SEA AND THEIR SIGNIFICANCE FOR PALEOCEANOGRAPHY
菲律宾海盆东北部晚始新世以来放射虫及其古海洋学意义
9.
THE DISCOVERIES OF THE LATE EOCENE PLANKTONIC FORAMINIFERA INTHE PEARL RIVER MOUTH BASIN AND THEIR GEOLOGICAL IMPLICATIONS
珠江口盆地晚始新世浮游有孔虫的发现及其地质意义
10.
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
11.
SOME NEW GENERA OF LATE CRETACEOUS TO EOCENE MICROPHYTOPLANKTON FROM WESTERN TARIM BASIN IN SOUTHERN XINJIANG
新疆塔里木盆地西部晚白垩世—始新世微体浮游植物的几个新属
12.
Primary Study on Quantitative Reconstruction of Middle-Late Eocene Climate in Jianghan Basin
江汉盆地始新世中、晚期古气候定量重建初探
13.
BIOTA AND DEPOSITIONAL ENVIRONMENT IN BEIJINGTIANJIN-BAXIAN AREA DURING LATE EOCENE AND EARLY OLIGOCENE
京津霸地区始新世晚期至渐新世早期的生物群及其沉积环境
14.
PALEOMAGNETIC STUDY OF SANSHUI BASIN IN GUANGDONG FROM LATE CRETACEOUS TO EOCENE AND ITS TECTONIC SIGNIFICANCE
广东三水盆地晚自垩世—始新世古地磁研究及构造意义
15.
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。
16.
Eocene series
始新统始新系始新-中新世
17.
A Study of Middle and Late Eocene Palynological Assemblages in Jianghan Basin and Their Environmental Significance
江汉盆地始新世中、晚期孢粉组合特征及其环境意义
18.
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。