寒武

网络释义

1.
Cambrian
他们一般将古生代分作寒武(Cambrian)、奥陶(Ordovician)、志留纪(Silurian)、泥盆纪(Devonian)、石炭纪(Carboniferous)以及 …
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2.
cambrian period
larry's blog--台湾土木工程词汇十八 ... cambridge model 模式 cambrian period 寒武 camber 拱 ...
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3.
Eocambrian
...，与寒武系之间多为整合接触，而与下伏地层之间...寒武（Eocambrian），门希考夫（Menchikoff）于1949...
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4.
Subcambrian
...层位为底寒武（Infracambrian），还有亚寒武（Subcambrian）等名称。
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例句

释义:
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1.
This rapid origin and diversification of animals is often referred to as "the Cambrian explosion"
如此迅速的动物起源和多样化被认为是“寒武纪大爆发”。
blog.sina.com.cn
2.
It was an important evolution and marked the end of transgression and regression cycle of the Cambrian and Ordovician in Tarim area.
这标志着塔里木地区寒武纪和奥陶纪海进海退旋回的终结。
www.ceps.com.tw
3.
"Plumes" from deep mantle do not operate in the modern Earth and did not operate in Precambrian time.
来自地幔深处的“热柱”，在现代地球上并无发生，其实，自寒武纪之后就不再发生。
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4.
For quite some time Cambrian remained just a scientific term concerned only by evolutionism scholars and paleontologists.
长期以来寒武纪仅仅是演化论学者和古生物学家所关心的科学名词。
bbs.translators.com.cn
5.
The beginning of the Cambrian era saw a widespread arrival of multi-cellular organisms, particularly in the form of sponges.
寒武纪时代的初期看了多细胞性的有机体普遍到来，特别以海绵的形式。
shaikhsiddiqui.com
6.
Chemical fossils (e. g. alkanes and porphyrins) are often the only evidence for life in rocks of PRECAMBRIAN age.
化学化石（烷烃和卟啉）是前寒武纪地层中生命存在的唯一证据。
plb.snnu.edu.cn
7.
This realization provided a big incentive for paleontologists to get out in the field and find fossils older than the Cambrian.
这项体认刺激了古生物学家走入田野，寻找比寒武纪更古老的化石。
dictsearch.appspot.com
8.
The Qiannan sag experienced the phase of the passive ocean margin rift basin in the early Cambrian, deposited a set of marine facies shale.
黔南坳陷早寒武世经历被动大陆边缘裂陷盆地演化阶段，沉积了一套海相黑色页岩。
www.cngascn.com
9.
As a result of rapid transgression in the Early Cambrian, a sequence of excellent source rock was widely developed in the Lower Cambrian.
寒武系，特别是下寒武统，由于寒武纪初期的快速海侵作用而在研究区域普遍发育烃源岩系；
www.ceps.com.tw
10.
They were formed in a dry tidal flat lagoon environment, and developed in the upper part of the Lower Cambrian.
震积岩形成于干燥的潮坪泻湖环境，发育在下寒武统的上部。
www.geojournals.cn