导航菜单

Cenozoic是什么意思_翻译中文_怎么读

Cenozoic

美式发音: [ˌsinəˈzoɪk] 英式发音: [ˌsi:nəˈzəuik]

adj.【地质学;地理学】新生代的

n.【地质学;地理学】新生代

中文释义:新生界的;中生代;新生代时期

中文释义

n.1.【地质学;地理学】新生代,新生界

adj.1.【地质学;地理学】新生代的,新生界的

n.1.the most recent era of geologic time, beginning about 65 million years ago, during which modern plants and animals evolved

1.新生代 cataclasite=catalastic rock 碎裂岩 = Cenozoic 新生界的 chemical property 化学性质 ...

3.中生代生动物(软体动物),没有留下什么化石给科学家发现作为物证。植物与动物的分途进化,不停地进行于古生代(Paleozoic)及

4.新生代时期 · Campus-Wide Information Systems 校园信息系统 (=Cenozoic) 新生界的, 新生代的 · =Chlorotrifluor Ethylene 三氟氯乙烯 ...

造句带翻译释义:,【地质学,地理学】新生代的,地理学】新生代,新生界的,中生代,新生代时期

1.Konggur in Late Cenozoic; the inflexion of every elevation rise gradient may be the dividing point of different uplift process.而每个抬升梯度的拐点,则对应着不同隆升过程形成海拔高度的分界点。

2.During the Cenozoic, tectonic deformation mainly occurred around the Ordos basin, resulting in the formation of the grabens.新生代时期,构造变形主要发生在鄂尔多斯盆地周缘,形成一系列地堑盆地。

3.Liaohe Basin is a rifted basin formed in the middle Cenozoic, faulting was the main tectonic movement of the basin.辽河盆地是形成于中新生代的裂谷型盆地,断裂活动是盆地的主要构造运动形式。

4.Langgu Sag is a Cenozoic sedimentary basin suffered a strong tectonic movement in the late stage, being of the properties of remnant basin.廊固凹陷是一个晚期构造运动强烈,具有残留盆地性质的新生代沉积盆地。

5.These terraces have been mostly folded and uplifted since the active tectonics in late Cenozoic.在最新构造活动的影响下,河流阶地普遍发生变形,遭受抬升。

6.The two tectonic systems are concrete manifestations of the active rifting and passive rifting mechanisms in the basin during the Cenozoic.这两种构造系统是盆地区新生代时期主动裂陷和被动裂陷两种作用机制的具体表现。

7.During the Cenozoic, the significant change of the global ecology system was the expansion of C4 plants.新生代以来,全球生态系统的重大改变之一为C4植物的扩张。

8.Local structural styles became more complicated due to the stacking of extensional structures and strike-slip structures of Meso-Cenozoic.局部由于受到中、新生代时期的伸展构造和走滑构造的叠加,构造样式变得更加复杂。

9.The cenozoic fracture cupped basin separates from north-east direction and east-west direction, and its form is controlled by active fault.新生代断陷盆地主要有北东向和东西向两组,其形态组成受控于活动断裂。

10.Therefore, the subsidence analysis presented here is truncated at the top of the continuous Cenozoic stratigraphic section.因此,这里提出的沉降分析被截断在连续的新生代地层剖面顶部。