Cenozoic信息详情
adj.新生界的（等于Cainozoic）
n.[地质]新生代；新生代之岩层
Cenozoic───n.[地质]新生代；新生代之岩层；adj.新生界的（等于Cainozoic）
Caenozoic───adj.新生代的；新生界的（等于Caenozoic）
Mesozoic───adj.中生代的；n.中生代
Neozoic───adj.新生代的
benzoic───adj.安息香的
cytozoic───adj.细胞内寄生的
endozoic───adj.动物内生的
entozoic───adj.内寄生的
Cainozoic───adj.新生代的（等于Cenozoic）；n.新生代（等于Cenozoic）
Between the last layer of Cretaceous rock and the first layer of Cenozoic rock, there is often a thin layer of clay.───在最后一层白垩纪岩石和第一层新生代岩石之间，常常有一层薄薄的粘土。
Plants and animals from the Mesozoic era were unable to survive in the Cenozoic era.───中生代的动植物在新生代无法生存。
Pre-Cenozoic basin structure, residual thickness and trichotomous property of basement are all shown by the impact.───撞击表明了前新生代盆地的结构，残余厚度和地下三分性。
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。
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。
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。
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。
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。
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。
The Bohai bay Basin is a Cenozoic rifting one.
Lakes developed widely Cenozoic era in central Tibetan Plateau.
Tens of Cenozoic basins, mostly small-sized in tramontane basins, are dispersely distributed in western Yunnan (west to Nujiang ri ver).
In Cenozoic, Chengbei 20 fault stops activity, Chengbei fault and Chengbei 30 north fault keep on developing, and Chengbei 30 south strike-slip fault and some new NE-trending faults start to develop.
Cenozoic tectonic activities are controlled by the eastward propagation of Tibetan Plateau uplift.
Fula sub basin is a Mesozoic and Cenozoic continental rifted basin, which is controlled by the Center Africa Strike slip fault.
Liaodongwan - Xialiaohe basin is a Cenozoic interior rifting basin.
The newest era is called Cenozoic beginning at 65 million years ago. It is the age of Mammals.
The triphibian chipping-rock sedimentary formation in Early Cenozoic in Adatan basin in western segment of east Kunlun Mt. was formerly considered to belong to "Low Tertiary".