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中元古界的英文

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"中元古界"怎么读用"中元古界"造句

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  • mesoprotozoic

例句与用法

  • The middle proterozoic granitoids was an intraplate type producted in transitinal crystalline basement before plate collision
    中元古界的花岗岩类是板块碰撞前过渡性结晶基底上局部熔融花岗岩类。
  • Characteristic of lithofacies paleogeography and sedimentary environment of the middle proterozoic wufushan group in jishan area , henan provin - ce , china
    河南箕山地区中元古界五佛山群沉积环境及岩相古地理特征
  • The kunyang group is distributed in the marrow and long belt constrained by the luzhijiang lithospheric fault and the xiaojiang - yimeng fault
    中元古界昆阳群分布于绿汁江岩石圈断裂和小江-易门断裂的夹持地带,呈狭长状展布。
  • The main diagenetic stage and relevant rock types are the middle proterozoic assemblage of gneissoid granodiorite - adamellite and the sinean schistosity diorates
    主要成岩期及代表性岩类有:中元古界为片麻状花岗闪长岩二长花岗岩,震旦纪为片理化闪长岩。
  • The mesoproterozoic wumishan formation in jixian , tianjin represents a succession of 300 - m thick carbonate strata , in which stromatolite biostromes and clotted bioherms are best developed
    天津蓟县中元古界雾迷山组为一套厚3000余米的碳酸盐岩地层,叠层石生物层和凝块石生物丘特别发育。
  • The main stratums contain gold element are yanlinggou team of qinling group and huoshengmiao team of erlangping group in sub - paleozoic , the lithologise that are the best related with gold mineralization are graphite marble and dolomite marble in yanlinggou team and splite marble in huoshenmiao team
    主要赋矿地层中元古界秦岭群雁岭沟组及下古生界二郎坪群火神庙组,与金矿化关系最为密切的岩性分别为雁岭沟组石墨大理岩、白云石大理岩及火神庙组细碧岩等。
  • Tianjin is located at north part of northern china plain , where is rich in thermal water in sedimentary basin . the main reservoir is carbonate rocks of the paleozoic and upper and middle proterozoic group , which contain thermal waters with temperature of more than 90 . the cap rock is cenozoic sedimentary rocks with thickness of more than 1000m , which contains thermal water with temperature from 25 to 70 in 13 sandstone layers . the temperature of thermal water is steady growth along with the deepen of basin . all thermal waters in different aquifers are medical mineral waters , which is conducive to good health
    天津位于华北平原的北部,那里的沉积盆地含有丰富的地下热水。主要的热储层为古生界和上中元古界的碳酸盐岩层,所含热水的温度略高于90盖岩层为新生界沉积层,在13个砂岩含水层中含有2570的热水。热水的温度随盆地深度的增加而增加。
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