本区具有出露良好的中新世地层。
Miocene formations (better: strata) are well-exposed in this area.
棱鳀属鱼类最早分化于中新世早期。
The divergence date of Thryssa species presented here is early Miocene.
中新世晚期，冲绳海槽和疏球岛弧形成。
Okinawa ocean trough and Ryukyu island arc were formed in late Miocene.
本区中新世末期气候事件与全球冷干气候事件一致。
The climate aridity event of Late Miocene can be correlated with the global climatic event.
中国西北地区，从中新世以来就有持续不断的风尘沉积。
Ever since the Miocene time, aeolian dust has been falling down over Northwestern China, forming the Loess Plateau.
伊朗晚中新世的几个地点新近发现了哺乳动物足迹化石。
Miocene mammalian footprints have been recently identified from several Late Miocene localities in Iran.
渐新世火山岩为高钾钙碱性系列，中新世岩石属于钾玄岩系。
Eocene lavas belong to high K Calc alkaline (HK CA) series and those of Miocene to shoshonite (SHO) series.
中新世晚期，NNE向断裂相对封闭，WNW向断裂相对开启。
The NNE_trending faults are relatively closed and the WNW_trending ones relatively opened during Late Miocene.
晚中新世以后，盆地进入浅海半深海沉积环境的裂后热沉降期。
After Late Miocene, the basin got into a post_rift thermal subsidence stage in a shallow to semi_deep sea environment.
本文记述了山东临朐山旺组(中新世中期)出产的两件鸟类化石。
Two fossil birds collected from Shanwang Formation, Middle Miocene (about fifteen million years ago), of Linqu, Shandong are here described.
通过应用多元分析的方法，对山旺中新世时期的植被进行了重建。
Using multivariate statistical analysis the palaeovegetation of the Shanwang profile has been reconstructed.
用来预测现代的人为全球变暖程度的气候模型显示，中新世的气温应该更低。
Climate models used to predict modern levels of man-made global warming, temperatures in the mid-Pliocene should have been lower.
喀什凹陷北部油砂的油源来自于侏罗系烃源岩，成藏期为中新世至上新世。
The oil source of oilsand in northern Kashi sag came from Jurassic hydrocarbon source whose reservoir-forming stage might be from Miocene to Pliocene.
该地区分布着两百余座大大小小的火山，形成于中新世、上新世和更新世。
There are more than 200 volcanic hills, mainly occurring in the Miocene, Pliocene and Pleistocene in the region.
我国最近发现的早中新世季风记录，对东亚季风系统何时形成又提出了疑问。
The recent discovery of monsoon records in early Miocene raised a question of the time when the East Asian monsoon system initiated.
包裹体等分析表明，盆地油气运移始于晚渐新世—早中新世，延续至第四纪。
Inclusion data shows that the migration of petroleum in the basin initiated from the Late Oligocene to the Early Miocene, up to the Quaternary.
最晚的化石记录分别发现于北美的中中新世、欧洲的上新世和亚洲的更新世。
Youngest occurrences were found from the Middle Miocene of North America, the Pliocene of Europe, and the Pleistocene of Asia.
盆地内某些区域，在层序iii之下，还存在层序v，为残留的中新世沉积物。
In some areas of the trough basin, sequence V, which is residual Miocene sediments, deposited beneath the sequence III.
晚渐新世—中中新世，盆地逐渐由断陷转为断拗，沉积范围不断扩大，整体处于海相沉积环境。
During the period from Late Oligocene to Middle Miocene, the basin changed from rifting to depression, and the depositional area continued to expand in the Marine environment.
第三阶段，中、晚中新世随着印度地块逐渐楔入欧亚板块内部，印支半岛的挤出运动进一步减弱。
The third phase, during the middle and the later Miocene, with the Indochina block intruding into Eurasia plate gradually, Indochina peninsula's extrusion slowed down further.
中新世以来，双河组（N1s）地层的褶皱走向为NE向，此期间盆缘主断裂变为左旋逆推性质；
Since the Miocene, the fold in the Shuanghe group (N1s) stroke in NE when the main fault on the basin rim changed into sinistral thrust.
中部背斜带中发育的构造主要为断层转折褶皱和少量断层传播褶皱，开始形成于中新世上新世中期；
The Central Anticline Zone composed of fault-band folds and a few fault-propagation folds, which started to form during Miocene to the middle stage of Pliocene.
在相同构造背景下，山旺盆地、包家河盆地和青山盆地的中新世对应层位的层序发育特征具有可比性。
With the same geological structural Settings, the Miocene sequence development of the Shanwang, Baojiahe, and Qingshan Basins are comparable.
南美洲南部的研究人员也提出了一些事实，让人相信在中新世时期，浅海的环境也存在于阿根廷内陆。
Researchers in southern south America have also made convincing cases that shallow Marine conditions existed in inland Argentina during the Miocene.
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。
Oligocene a geological epoch in the Tertiary, between Eocene and Miocene, lasting from about 38 to 25 million years ago.
研究注意到在2个结壳中都没有发现可信的晚渐新世到中新世的化石记录，在个别层位之间存在着沉积间断。
This study notes that no reliable Late Oligocene to Miocene nannofossil markers were found in these 2 crusts. Furthermore, sedimentation hiatus was observed.
矿区出露中朱罗统叶巴组火山次火山沉积岩、古新世黑云母花岗斑岩、中新世二长石英斑岩以及渐新世花岗斑岩。
The middle Jurassic Yeba formation volcanics, Paleocene biotite granite porphyry, Miocene quartz monzonite and Oligocene granite porphyry could be found in the ore field.
而在大约3千4百万年前的渐新世的欧亚大陆上达到顶峰，在大约1千万年前中新世的欧亚大陆和非洲大陆又再次达到顶峰。
It peaked in the Oligocene Epoch around 34 million years ago in Eurasia, and again in the Miocene Epoch about 10 million years ago in Eurasia and Africa.
珠江口盆地晚渐新世至早中新世所形成的珠江组和珠海组是盆地内烃类的重要储集层，在珠三坳陷中珠江组砂岩比珠海组的更为重要。
The sandstones of Zhujiang and Zhuhai formations, which were formed during the Late Oligocene and Early Pliocene, are major reservoir for hydrocarbon in Pearl River Mouth Basin.
珠江口盆地晚渐新世至早中新世所形成的珠江组和珠海组是盆地内烃类的重要储集层，在珠三坳陷中珠江组砂岩比珠海组的更为重要。
The sandstones of Zhujiang and Zhuhai formations, which were formed during the Late Oligocene and Early Pliocene, are major reservoir for hydrocarbon in Pearl River Mouth Basin.
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