CENOZOIC

新生代
常用释义
新生代

扩展信息

新生代
新生代Cenozoic) 是地球历史上最新的一个地质时代,它从6600万年前开始一直持续到今天。随着恐龙的灭绝,中生代结束…
新生界的
地质词典_百度文库 ... cataclasite=catalastic rock 碎裂岩 = Cenozoic 新生界的 chemical property 化学性质 ...
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
新生代时期
新生代时期 (Cenozoic) 是地球历史上最新的一个地质时代,从6400万年前开始一直持续到今天,随着恐龙的灭绝,中生代结束…
新生代的
... · 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 ...

例句

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。

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。

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。

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。

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。

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。

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。

trending long and narrow depression located in the north of the Tarim Basin and is dominated by Meso-Cenozoic strata.

库车坳陷是塔里木盆地北部一近东西走向的狭长坳陷,以中新生代地层为主。

通过初步分析,指出了北方主要中新生代盆地砂岩型铀矿的找矿方向。

This Late Cretaceous deformation determined the complicated contact relationships of Cenozoic and Early-Cenozoic sequences.

现今新生代层序和下伏层序的复杂接触关系主要是由该期构造运动决定的。

Mount Wutai is a typhical example of the Cenozoic continental extension and of the fault block orogeny.

五台山为早期寒武纪地壳中新生代伸展、断块造山活动的典型代表

Carbonaceous siliceous-argillite rock type uranium deposits are mainly located near Meso-Cenozoic sedimentary basins(in brief, red basin).

碳硅泥岩型铀矿床主要产于中新生代沉积盆地(简称为红盆)的附近。

中新生代辽河盆地的形成和发展受控于多期区域应力场变化。

In Tengchong, the diatom was occurred in several Cenozoic lake basin formed by the intensive structural movement after Eogene.

古近纪之后,强烈的构造运动在腾冲形成数个新生代湖盆,成为硅藻生存场所。

Rupture zone controls the North-South differences of cenozoic diastrophism and present lithosphere movement of Fujian Province.

断裂带控制了福建地区新生代地壳变形和现今地壳运动的南北差异。

震波相分析指出,新生代后期之沈积物主要在近海环境生成。

新生代地层中砾岩砾石成分稳定,以变质岩和沉积岩成分居多,岩浆岩很少;

The Xiaoxia anticline in the northeastern Qinghai-Tibetan Plateau forming during the Cenozoic is one basement-involved fold.

青藏高原东北部小峡背斜是一个新生代发展起来的基底卷入型背斜。

ARE THE FAULTS CONTROLLING MESO-CENOZOIC BEARING OIL AND GAS BASINS IN EASTERN CHINA TENSILE FRACTURES?

中国东部某些中、新生代含油气盆地与部分北东向正断层成因分析?

新生代全球气候变化总体呈现随时间变凉的趋势,其间伴随冷暖交替。

中国北东部中新生代盆地是地浸砂岩型铀矿的主要勘查区。

Wushi Sag is a superimposed basin of two stage foreland basins of Mesozoic and Cenozoic.

乌什凹陷为中新生代两期前陆盆地叠加形成的叠合盆地。

Yitong basin is a strike-slip stretching basin which is controlled mostly by the strike-slip fault of the north-west boundary in Cenozoic.

伊通盆地主要是受西北缘走滑断裂控制的新生代走滑-伸展盆地;

青海东部诸多中新生代断陷盆地中广泛分布着陆生红色碎屑岩地层。

Helium isotope compositions of the mantle-derived xenoliths and megacrysts from the Cenozoic basalts in Hannuoba were measured.

对该地区新生代玄武岩中幔源包体和高压巨晶的氦同位素进行了初步研究。

郯庐断裂带鲁皖段新生代玄武岩形成机制的稀土判别。

Among them the Precambrian and Cenozoic eras are the main metallogenic epochs in the world.

就全球而言,前寒武纪和新生代是金矿的重要成矿期。