oligocene

oligocene

美 [ˈɒlɪgoʊˌsin] 　英 [ɔˈliɡəusi:n]

• n.【地】渐新世(的)；渐新统(的)
• 网络渐新世时期；新渐世；渐新世界

英汉解释

n.	1. 【地】渐新世(的);渐新统(的)

英英解释

n.	1. the epoch of geologic time, 38 million to 24 million years ago, during which primates first appeared

例句

any of many extinct cats of the Old and New Worlds having long sword like upper canine teeth; from the Oligocene through the Pleistocene.

东半球许多已经灭绝的猫科动物，其上犬齿形如长剑；生活在从渐新世经由更新世时期。

As in the Oligocene before it, grasslands continued to expand and forests to dwindle in extent.

在先前的渐新世，草地的面积增大，森林的面积减少。

The west side of the lake offers much older fossils from the Miocene, Oligocene and Cretaceous eras (including dinosaur remains).

而盆地西部的化石，年代则更古老，从含有恐龙遗迹的白垩纪，到渐新世与中新世。

Hundred years, Quanzhou experienced many historical changes, the new interactive air-filled history of old customs, culture Oligocene.

百多年来，泉州经历多次历史变革，新风旧俗交互递嬗，风气渐新。

the Upper Cretaceous was in the higher base level, which developed fan delta- lacustrine facies until late Oligocene.

上白垩统基准面快速抬升，沉积区整体处于湖泊-扇三角洲沉积体系，一直持续到古近系渐新统晚期。

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。

In the Ostra Field, Venezuela, oil is produced from lenticular sandstone beds of the Oligocene oficina Formation.

委内瑞拉奥斯特拉油田的产油层，为渐新世奥菲西那组透镜状砂岩层。

Oligocene A geological epoch in the Tertiary, between Eocene and Miocene, lasting from about 38 to 25 million years ago.

渐新世纪第三纪始新世与中新世之间的地质纪元，大约从三千八百万年持续到二千五百万年前的一段时间。

Baiyun Movement, a Great Tectonic Event on the Oligocene-Miocene Boundary in the Northern South China Sea and Its Implications

白云运动：南海北部渐新统-中新统重大地质事件及其意义

Occurrence of Palygorskite in Late Oligocene in Linxia Basin and Its Geological and Climatic Indicator

临夏盆地晚渐新世沉积物中坡缕石的发现及其环境气候意义

Characteristics of Clay Mineral in South China Sea since Oligocene and Its Significance

南海渐新世以来粘土矿物的演变特征及意义

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

Evolution of Atlantic Thermohaline Circulation: Early Oligocene Onset of Deep-Water Production in the North Atlantic

大西洋温盐循环的演变：早渐新世北大西洋深水开始形成

Subsidence stage from Oligocene to Mid-Miocene, fault block activation only occurred in early-middle Oligocene;

渐新世-中中新世坳陷沉降阶段，在渐新世早中期存在继承性断块活动；

Evidence for an Earliest Oligocene Ice Sheet on the Antarctic Peninsula

南极半岛渐新世早期冰盖的证据

Tectonic Events Indicated by Late Oligocene Slumped Deposits from the South China Sea

南海晚渐新世滑塌沉积指示的地质构造事件