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precambrian中文是什么意思

  • adj.
    【地质学;地理学】前寒武纪的。
    n.
    〔the Precambrian 〕 前寒武纪。

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  • 例句与用法
  • The texas state capital sity straddles the line between two geologic provinces - to the west is the uplifted plateau of cretaceous limestones and exposed precambrian llano uplift , while the lowland bladk prairie country stretches eastward for miles
    西部是白垩质的石灰石突起的高处地带和暴露的precambrian llano突出处,而低处的black prairie直向东部扩展数里。
  • The term of the previous precambrian metallogenic domain is not adopted , and the precambrian metallogeny should be discussed as the metallogeny of the basement in the relevant paleo - asiatic , qinling - qilian - kulun and tethys metallogenic domains
    对于前寒武纪成矿作用地区,文章不以“成矿域”称之,其成矿作用置于古亚洲、秦祁昆和特提斯诸成矿域中以基底成矿作用方式讨论之。
  • Some mistakes of " super - contacting " or " superimposing " remained in the late precambrian stratigraphic sequence in southern liaoning province and the north of jiansu and anhui provinces , and between penglai group in eastern shandong and tumen group in western shandong
    摘要辽南、苏皖北部地方的晚前寒武纪地层层序,以及鲁东蓬莱群与鲁西土门群的上下层位,存在著“叠接”与“叠置”的错误。
  • And , at several spots on the planet , the ediacaran lagerst ? tten , named after the ediacara hills of australia where the first example was found , harbor strange precambrian soft - bodied fossils and animal burrows , including evidence for early bilaterians
    而分布在地球上数个地区的艾迪卡拉特异埋藏点(命名自首次发现的澳洲艾迪卡拉山) ,里面藏有奇妙的前寒武纪软体化石与虫穴,包括早期两侧对称动物的证据。
  • It is pointed out that there exist abundant precambrian mineral resources in china , forming numerous large - superlarge iron , copper , lead , zinc , nickel , gold , ree , manganese , graphite , magnesite , talc , boron , phosphorus , pyrite , rutile and vermiculite deposits
    指出中国前寒武纪蕴藏著丰富的矿产资源,形成了众多的铁、铜、铅锌、镍、金、稀土、锰、石墨、菱镁矿、滑石、硼、磷、硫铁矿、金红石、蛭石等大型超大型矿床。
  • It is believed that the distribution of gold deposits in fujian is controlled by regional deep - seated structure and precambrian volcanic flysch formation containing charcoal is main gold source rock . the accumulation of gold is closely related with yanshan granitic magma intrusion
    金矿空间分布受一定的区域深部构造单元所制约,前寒武系富含炭质的火山复理石建造是福建省金矿的主要矿源岩,金的富集成矿与燕山期花岗岩类岩浆侵入作用密切相关。
  • The basement of the basin is consist of precambrian crystal basement and paleozoic folding basement , while the cover has undergone the evolution of intra - continental rife in permian , down warped basin in triassic - cretaceous period and inter - mountains basin in tertiary . the main sediments are huge - thick volcanic rock , shallow intrusive rock and tuff in early permian , dark mudstone , marl and muddy dolostone in lucaogou formation in middle permian , huge thick volcanic rock , intruder in tiaohu formation in middle permian , miscellaneous sandy gravel , sandstone and gray mudstone in triassic ( the red is under the gray , and huge - thick dark gray , gray sandy gravel , sandstone , mudstone with coal layer in jurassic
    盆地基底由前寒武纪结晶基底和古生代褶皱基底组成,盆地盖层则经历了二叠纪的裂谷盆地、三叠纪?白垩纪的坳陷盆地和第三纪后的山间盆地的演化过程。盆地主要沉积了下二叠统巨厚火山岩、浅成侵入岩和凝灰岩;中二叠统芦草沟组的暗色泥岩、泥灰岩、白云质岩石以及条湖组的巨厚层火山岩、侵入岩;三叠系杂色砂砾岩、砂岩及灰色泥岩(下红上灰) ;以及侏罗纪厚层深灰、灰色砂砾岩、砂岩、泥岩夹煤层。
  • Eight aspects related to the study of early precambrian metamorphic stratigraphy are dealt with in this paper : general situation of the study ; complexity of the stratigraphy and difficulties of the study ; thoughts and methods of the study ; division of rock suite , rock group and complex rock ; researches on important regional discordances ; types and characteristics of protolith and recovery of palaeoenvironment ; correct differentiation of the metamorphic strata , ttg rock system and other metamorphic plutonic rocks ; determination of the ages of the metamorphic strata
    摘要主要论述了与早前寒武纪变质地层(学)有关的8个方面的问题:早前寒武纪变质地层的研究概况;早前寒武纪变质地层的复杂性和研究难度;早前寒武纪变质地层研究的思路和工作方法;早前寒武纪变质岩石地层单位岩群、岩组和杂岩的划分问题;重要区域性不整合的研究;鉴定变质地层的原岩类型、岩石性质和恢复古环境;正确区分变质地层和ttg岩系以及其他变质深成岩;变质地层时代的确定。
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  • 百科解释
The Precambrian (Pre-Cambrian) is the name which describes the large span of time in Earth's history before the current Phanerozoic Eon, and is a Supereon divided into several eons of the geologic time scale. It spans from the formation of Earth about 4570 Ma (million years) ago to the beginning of the Cambrian Period, about Ma, when macroscopic hard-shelled animals first appeared in abundance.
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