• The origination of the magma is related with the dehydration of the subducting plate of the Paleozoic Tethys Sea.

    岩浆起源古生代特提斯海俯冲板块的脱水有关。

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  • They are mainly living in the Paleozoic.

    它们主要生活古生代

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  • Its age is Sinian early Paleozoic to Devonian.

    时代主要震旦纪—古生代至泥盆纪。

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  • Paleozoic to Quaternary sediments well developed in the Southern Yellow Sea.

    黄海地区发育古生界第四沉积

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  • This was the end of the Permian period, and of the era of life called the Paleozoic.

    就是二叠纪以及整个古生代终结

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  • The stratigraphic column in this district includes all the Paleozoic formations.

    这个地区地层包括全部古生代岩系

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  • Zhungaer basin is a composite and superimposed foreland basin since late Paleozoic.

    准噶尔盆地古生代以来多期形成的复合叠加前陆盆地。

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  • This was one of the first fossil algae to be described as such from Late Paleozoic rocks.

    最早化石藻类之一描述了这种古生代岩石作为

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  • The strata are mainly late Paleozoic-Mesozoic with widely distribution of Triassic strata.

    主要发育古生代—中生代地层,尤其是三叠系广泛分布

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  • This paper applies the theory of finite strain to the study of Paleozoic structures in Chengdao region.

    该文有限变形理论应用埕岛地区古生构造变形研究中。

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  • The communities of Paleozoic plants congregated at the water's edge and began to colonize the Earth's surface.

    大量古生代植物聚集水域边缘逐渐蔓延地球各个角落。

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  • The exploration and research levels of Middle Paleozoic Marine strata are low in West Pingle Depression.

    乐坳陷西部中古生界海相区块勘探研究程度低。

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  • The early Paleozoic strata can be divided into the Cambrian Hulan Group and the Ordovician Liaoyuan Group.

    吉林槽区的早古生代地层分为武系呼兰奥陶系辽源群。

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  • The Ordos basin is a large Mesozoic intracontinental basin superimposed on the Paleozoic North China craton.

    鄂尔多斯盆地叠加华北古生代克拉通台地之上的中生代大型内盆地。

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  • Several nappes have been found in the late Paleozoic and Mesozoic coal-bearing basins in southeastern Hunail.

    湖南省东南部古生代中生代盆地多处发现推覆构造。

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  • There are three types of mineralization fluid in Later Paleozoic sedimentary basin in North-Guangdong province.

    粤北古生代沉积盆地存在三种类型矿化流体

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  • The Phanerozoic is divided into three eras -starting with the earliest, these are the Paleozoic, Mesozoic, and Cenozoic.

    生宙可划分三个时期——依次经历古生代、中生代新生代。

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  • The Lower Paleozoic reservoir is Majiagou formation's putty crystal dolomite and powder crystal dolomite primarily.

    古生界储层主要以马家沟组的泥白云岩晶白云岩为主。

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  • The Phanerozoic is divided into three eras — starting with the earliest, these are the Paleozoic, Mesozoic, and Cenozoic.

    生宙可划分三个时期——依次经历古生代中生代新生代。

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  • Most of the fossils seen in Paleozoic rocks are invertebrate animals lacking backbones, such as corals, mollusks and trilobites.

    大部分古生代岩层中发现化石都是没有脊骨无脊椎动物例如珊瑚、软体动物和三叶虫。

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  • The porphyry copper metallogenic belt in Beishan area belongs to the Paleo Asia paleozoic porphyry copper metallogenic province.

    甘肃北山岩型铜矿成矿属于世界古亚洲古生代斑岩带成矿域。

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  • Upper Paleozoic natural gas reservoir of Ordos Basin consists of low-permeability sandstone which bears typical secondary porosity.

    鄂尔多斯盆地上古生界天然气集体是一套次生孔隙为主低渗透砂岩

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  • This paper discusses the filling succession and evolution of the NW-trending Paleozoic Shuicheng-Ziyun aulacogen in western Guizhou.

    研究了贵州西部古生代发育起来北西向水城-紫云裂陷槽盆的充填序列演化

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  • The optical anisotropy of zooclast graptolite in some Paleozoic strata of China has been studied using reflectance cross-plot analysis.

    应用反射率十字图解研究了中国部分地区下古生界地层中动物有机碎屑笔石光学各向异性

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  • Carboniferous: of, belonging to, or denoting a geologic division of the Paleozoic Era following the Devonian and preceding the Permian.

    石炭纪,石炭系的:(属于表示)地质上的一个分段,即紧跟着泥盆纪早于二叠纪古生代的。

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  • This paper divides the Paleozoic - Middle-Upper Proterozoic marine basins into the closed bearing basin type and open relief basin type.

    本文古生界一中、上元古界海相盆地分为封闭型承压盆地开启泄压盆地两大类型。

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  • The tectonic nature of different regions in China in the Early and Late Paleozoic, Mesozoic and Cenozoic coal-forming periods is different.

    中国古生代中生代新生代大地构造性质各个地区不同。

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  • Some organisms have persisted with so little change that specimens living today are quite similar to their Paleozoic or Mesozoic ancestors.

    有些生物一直很少变化以至生存至今的生物它们古生代中生代祖先十分相象。

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  • Some organisms have persisted with so little change that specimens living today are quite similar to their Paleozoic or Mesozoic ancestors.

    有些生物一直很少变化以至生存至今的生物它们古生代中生代祖先十分相象。

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