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middle ordovician中文是什么意思

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用"middle ordovician"造句"middle ordovician"怎么读"middle ordovician" in a sentence

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  • 中奥陶世

例句与用法

  • Characteristics and origin of dolostones in yingshan formation , lower and middle ordovician , north of central tarim basin
    塔中北部中下奥陶统鹰山组白云岩特征及成因
  • The main controlled factors of heterogeneity of middle ordovician majiagou 51 - 4 reservoir in jingbian buried platform and its periphery area , ordos basin
    4亚段储层非均质性主要控制因素
  • This paper is a continuation of the papers on lithofacies palaeogeography of the early , middle and late cambrian and the early and middle ordovician
    摘要本文是笔者等的中国早、中、晚寒武世和早、中奥陶世岩相古地理诸文的继续。
  • From the late middle ordovician to the end of ordovician , the cephalopods , gastropods and corals in the erlangping trough , and the conodonts , coral , brachiopods , cephalopods as well as trilobites in the xichuan shelf were from the north china province
    在中奥陶世晚期至奥陶纪末,二郎坪海槽的腹足类、头足类和珊瑚与浙川陆棚的牙形石、珊瑚、腕足类、头足类和三叶虫均属华北生物省。
  • 2 . tazhong ancient uplift originated from normal fault in paleozoic , hydrocarbon formed in ordovician period , structure reverse made tazhong uplift form from the middle ordovician period to the late ordovician period , and it provided geologic background for the deposit of silurian - devonian stratum . tazhong uplift formed at the end devonian , ancient reservoir was destroyed and asphaltum sandstone formed , structure deformation more destroyed ancient reservoir in early permian , after then the major of structure deformation is regulation
    塔中隆起源于早古生代拉张背景下的正断层,寒武-奥陶纪为其烃源岩形成的重要时期;早奥陶世末-晚奥陶世末的构造反转是塔中隆起的主要形成期,同时也为志留系形成地层及复合圈闭提供了古地理背景;志留?泥盆纪塔里木盆地南北缘均转为活动大陆边缘,形成了大量的断裂和不整合;泥盆纪末塔中鼻状隆起基本定型,古油藏遭受破坏,形成了沥青砂岩;早二叠世晚期的构造变形使古油藏遭受进一步的破坏;二叠纪后构造变动主要以调节为主。
  • From the cambrian to the early middle ordovician , the cambrian radiolaria and the early ordovician conodonts of the erlangping trough in the northern part of eqm , and the cambrian trilobites and early ordovician conodonts as well as cephalopods of the northern xichuan shelf in the southern part of eqm belonged to the south china province , while the cambrian trilobites and the early ordovician conodonts of the southern xichuan shelf belonged to the south china province with some elements of the north china province
    在寒武纪至中奥陶世早期,东秦岭北部二郎坪海槽的寒武纪放射虫和早奥陶世牙形石与东秦岭南部浙川陆棚北部的寒武纪三叶虫、早奥陶世牙形石和头足类属华南生物省,而浙川陆棚南部的寒武纪三叶虫和早奥陶世牙形石属于华南生物省,兼有华北生物省分子。
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