miocene
美 [ˈmaɪəˌsin] 
英 [ˈmaiəsi:n]
- adj.【地质学；地理学】第三纪中新世的
- n.【地质学；地理学】第三纪中新统
- 网络中新世时期；中新世第三纪；新生代第三纪中新世
英汉解释
英英解释
例句
At the time the nuts were hoarded, the Miocene period, crocodiles, apes and palm trees were all common to western Europe.
根据研究，在坚果被贮藏的哪个时期，也就是中新世纪的时候，在西欧随处可见猿猴和棕榈树！
The formation of the regional hydrothermal deposits was improved by the transition of tectonic system around the Miocene.
中新世前后的构造转折促进了全区热液型矿床的形成。
The island is of volcanic origin, made of basaltic tuff and lava dating from the Miocene epoch.
这个岛起源于火山喷发，由玄武岩、凝灰岩和熔岩在中新世形成。
A study of fossil teeth from grazing animals sheds light on what Europe was like during Late Miocene times.
一项关于食草动物牙齿化石的研究给人们了解中新世晚期的欧洲带来了希望。
During the middle Miocene, northeastern Spain, where the fossils were discovered, was humid and moderately warm, Dr. Abella said.
阿韦利亚表示，中新世中期，西班牙东北部是一片潮湿、适度温暖的地区，这些化石就是在那里发现的。
In the Miocene seas, kelp forests made their first appearance and soon became one of Earth's most productive ecosystems.
而在中新世海洋巨藻丛林开始出现并且很快成为生物系统中多产的一链。
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。
The Amazon dolphin, Inia geoffrensis, parted company with its oceanic ancestors about 15 million years ago, during the Miocene epoch.
亚马逊河豚，大约1500万年前，中新世时期，和其海洋祖先分道扬镳。
The apes arose and diversified during the Miocene epoch, becoming widespread in the Old World.
在中新世猿类动物兴起并向多样化发展，广泛分布在这个远古的世界上。
The first movement of the salt began in the early Miocene, when the salt structure grew slowly and stably.
厘定库车坳陷盐构造初始形成时间在中新世早期，盐构造早期生长缓慢而稳定；
The volcanic rocks in this region were formed no later than the Late Miocene. Considerable magmatic activity appeared during Pleistocene.
火山岩的生成年代不晚于中新世晚期，至更新世岩浆活动尤为强烈。
Here, the Miocene Hoh Formation is tilted about 45 degrees to the right (south); the overlying marine terrace gravels are horizontal.
华盛顿州奥林匹克海滨角度不整合，这儿，中新世的Hoh组大致向右（南）以45°角倾斜；上覆的海岸阶地砂砾是水平的。
therefore , the thesis thinks wudaoliang group and suonahu formation are the outcome of the miocene epoch.
因此，论文认为五道梁群和唢呐湖组都是中新世时期的产物。
Chang, Stanley(1968) Regional stratigraphic study of the lower Miocene formations in northern Taiwan. Petroleum Geology of Taiwan, 6, 45-70.
张锡龄（1968）台湾北部下部中新世地层之区域性研究。台湾石油地质，第6号，第45-70页。
Volatiles from Two Gymnosperm Fossils: Miocene Leaves of Metasequoia glyptostroboides and Early Cretaceous Seed Cone of Pityostrobus spp.
中新世水杉叶片和白垩纪松型球果化石中的挥发性成分。
LH4-1 Oilfield is a heavy oil field developed from the basis of the bioherm of Miocene Zhujiang Formation.
LH4-1油田是在新近系中新统珠江组生物礁基础上发育起来的稠油油田。
Gas chimney is the main pathway for gas migration in Qiongdongnan basin after middle Miocene.
在中中新世后，气烟囱是琼东南盆地气体向上运移的通道。
Miocene formations (better: strata) are well-exposed in this area.
本区具有出露良好的中新世地层。
Finally, after contractive uplift in Miocene, Present Junggar Basin was formed in the end.
最后在中新世时萎缩上隆，形成了现代的准噶尔盆地。
It is the product of Miocene porphyry-skarn metallogenic system in the Jiama copper polymetallic deposit, Tibet.
是西藏甲玛中新世斑岩-夕卡岩成矿系统的产物。
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。
Early Miocene is the key period of Tibetan Plateau uplift.
中新世是青藏高原整体隆升和环境变化的关键时期。
Miocene series is not mature because of buried very shallow.
中新统烃源岩由于埋深较浅，基本未成熟。
The strata of Miocene and Pliocene in the study area deposit in the deepsea plain and toe of slope.
中新世至上新世，研究区发育深海平原和陆坡坡脚沉积。
Chou, J. -T. (1980) Stratigraphy and sedimentology of the Miocene in western Taiwan. Petroleum Geology of Taiwan, 17, 33-52.
周瑞炖（1980）台湾西部中新统之地层学及堆积学研究。台湾石油地质，第17号，第33-52页。
Chiu, H. -T. (1972) Miocene stratigraphy of the Nantou area, central Taiwan. Petroleum Geology of Taiwan, 10, 159-177.
邱华灯（1972）台湾中部南投区域中新世地层之层位。台湾石油地质，第10号，第159-177页。
Magnetostratigraphy and Sedimentology of the Eolian Deposits Since the Late Miocene in Northern China and the Paleoclimatic Implications
晚中新世以来中国北方风成沉积的磁性地层学和沉积学研究及其古气候意义
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
Planktonic Foraminifer and Oxygen Isotopic Evidence of a Late Miocene Western Pacific Warm Pool
晚中新世西太平洋暖池的浮游有孔虫和氧同位素证据
Discovery of Mantle Xenoliths Bearing Miocene Potassium-Rich Olivine Basalt and Its Significance in Siziwangqi Area, Inner Mongolia
内蒙古四子王旗东八号中新世含深源捕虏体富钾橄榄玄武岩的发现及其意义
Types and Origin of Diatomaceous Laminae of the Miocene Shanwang Formation in Linqu, Shandong Province
山东山旺中新世硅藻土的纹层类型及成因
Eolian Sand Deposition and Its Environmental Significance inLinxia Basin Since Middle Miocene
临夏盆地晚中新世以来的风沙沉积及环境意义
Braided-river deltaic sediments of the Miocene Anju'an Formation in the Southwest depression, Tarim basin
塔里木盆地西南坳陷中新统安居安组辫状河三角洲沉积
An analysis of creation conditions for Miocene stratigraphic and lithologic traps in Huizhou area, Pearl River Mouth basin
珠江口盆地惠州地区中新统地层岩性圈闭形成条件分析
The Discovery of Miocene Aeolian Sediments and Its Paleoenvironmental Significance in East China
中国东部中新世风尘沉积的发现及其研究意义
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；
Structure reversion stage in Late Miocene, formed the huge reversal anticline, NNE and EW trend cover fault;
晚中新世构造反转阶段，形成大型反转背斜、北北东向和近东西向盖层断层；
Study on Miocene stromatolites genesis and related paleo-environment in Qaidam basin
柴达木盆地中新世叠层石成因与古环境研究
Paleoelevation reconstruction of Red River drainage areas in Western Yunnan Plateau since Miocene
中新世以来滇西高原内红河流域区的古高程反演
Magnetostratigraphy of a late Miocene-Pliocene loess-soil sequence in the western Loess Plateau in China
在中国西部黄土高原中新世纪-上新世纪晚期黄土序列的磁层图示法
