1.
Beibu Wan Basin was a lake in the middle Eocence-Lower Oligocene.
北部湾盆地在中始新世至早渐新世是一个湖泊。
2.
After the early Oligocene,the Nansha massif was amalgamated with the Borneo massif. Then the neritic-bathyal environment gradually predominated in the Beikang basin.
早渐新世后,南沙地块与婆罗洲地块拼贴,北康盆地逐渐处于浅海-半深海环境。
3.
The deposits of the Oligocene Epoch.
渐新统渐新世的沉积物
4.
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
5.
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
6.
OLIGOCENE SANHE FLORA IN LONGJING COUNTY OF JILIN, NORTHEAST CHINA
吉林龙井渐新世三合植物群(英文)
7.
Slowly these Neolithic people spread over the warmer parts of the world;
渐渐地，这些新石器时代的人类遍布世界较暖和的地区；
8.
A NEW LOWER CAMBRIAN TRILOBITE FROM KEPING,W.SINKIANG
新疆柯坪早寒武世的一个三叶虫新属
9.
GLOBAL CLIMATE EVENT AT THE EOCENE-OLIGOCENE TRANSITION: FROM GREENHOUSE TO ICEHOUSE
始新世—渐新世界线的全球气候事件:从“温室”到“冰室”
10.
MINERALOGY IN STRATA AROUND THE BOUNDARY BETWEEN EOCENE AND OLIGOCENE AT SITE 573 IN EAST PACIFIC
东太平洋地区573孔始新世末—渐新世初地层矿物学
11.
THE CHARACTERISTICS AND REEs GEOCHEMISTRY IN THE STRATA FROM LATE EOCENE TO EARLY OLIGOCENE IN SITE 573, THE EASTERN PACIFIC
东太平洋573孔始新世末渐新世初地层特征及稀土元素地球化学
12.
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
13.
Geochemical Features of the Meteorite Impact Around Eocene/ Oligocene Boundary Layer in Central Eastern Pacific Region
东太平洋中部始新世/渐新世界线陨石撞击的地球化学证据
14.
Middle eocene-oligocene climatic changes recorded by sedimentary colors in the Xining Basin,in northeastern Tibetan Plateau,NW China
青藏高原东北部西宁盆地中始新世-渐新世沉积物颜色与气候变化
15.
DISCOVERY ON THE COLUMN-LIKE FOSSILS FROM THE EARLY EARLY CAMBRIAN OF SOUTH SHAANXI
陕南早寒武世早期管柱状生物化石新发现
16.
Oligocene erosion had truncated the sediments draped over the dome.
覆盖于穹丘上的沉积岩为渐新世侵蚀所截削。
17.
Regional tectonic conditions for intensive subsidence of the middle Bohai Sea since Oligocene
渤海中部渐新世以来强烈沉陷的区域构造条件
18.
FOSSIL LEPORIDS FROM THE MIDDLE OLIGOCENE OF ULANTATAL, NEI MONGOL
内蒙古阿左旗乌兰塔塔尔中渐新世的兔科化石