二叠纪的的英文

• dyassic
• permian

• "的"英文翻译    4次方是 The fourth power of 2 i ...
• "二叠纪" 英文翻译 :    dias; permian period
• "二叠纪 二叠系" 英文翻译 :    dias; dyas
• "二叠纪；二叠系" 英文翻译 :    dyassic
• "二叠纪时期" 英文翻译 :    permian period million years ago
• "二叠纪粘土" 英文翻译 :    permian clay
• "石炭二叠纪" 英文翻译 :    permo-carboniferous period
• "晚二叠纪" 英文翻译 :    grauliegendes
• "下二叠纪" 英文翻译 :    saalian
• "中二叠纪" 英文翻译 :    saxonian
• "三叠纪的" 英文翻译 :    triassic
• "二叠纪-三叠纪灭绝事件" 英文翻译 :    permian-triassic extinction event
• "大石炭纪；石炭纪及二叠纪" 英文翻译 :    anthracolithic period
• "二叠纪盆地皇家信托公司" 英文翻译 :    permian basin royalty trust
• "方法预测二叠纪湾的石油产量" 英文翻译 :    how hubbert method fails to predict oil production in the permian basin
• "三叠纪" 英文翻译 :    jura-trias; triassic peorid; triassic period
• "二叠分" 英文翻译 :    stacked
• "二叠体" 英文翻译 :    bigeminum; coporabigemina; corpora bigemina
• "二叠系" 英文翻译 :    dias; dyassic; permian period; permian system
• "大冶统(三叠纪)" 英文翻译 :    tayeh series
• "三叠纪中期" 英文翻译 :    ladinic
• "上三叠纪" 英文翻译 :    upper triassic
• "晚三叠纪" 英文翻译 :    lufeng
• "早三叠纪" 英文翻译 :    chinglung limestone
• "中三叠纪" 英文翻译 :    schlern(dolomite

• According to the content of mgo , emeishan basalt can de divided into high - mg ( mgo > 12 % ) volcanic rock and lower - mg ( mgo < 12 % ) basalt
  该区二叠纪的火山岩依据mgo 12可分为两个岩石化学类型：低镁火山岩即峨眉山玄武岩；高镁火山岩。
• This extensional activity is similar to the basin - and - range province of western america , and can be thought as an intra - continental tectonic system
  此外，扬子地块西缘二叠纪的大陆伸展作用类似于美国西部的盆岭区，总体表现为大陆板块陆内构造体制。
• Based on the variation of light / heavy mineral components of sedimentary rocks , the typomorphic characteristics of various debris , the cathodoluminescence color of quartzes , the direction of paleocurrent and the extension of sedimentary facies , two source direction of the studied area in carboniferous and permian can be recognized , one is in bayanwusu , wulan ' ge ' er and hetaoyinshan area north of hangjinqi in the north margin of ordos , another is alashan area in the northwest margin of ordos
  在深入研究本区沉积岩轻、重矿物组分的变化、各种岩屑的标型特征、石英阴极发光颜色、古水流方向及沉积相带展布等基础上，认为研究区石炭?二叠纪的物源方向主要有两个，分别为：北缘杭锦旗以北的巴彦乌苏、乌兰格尔及河套阴山地区；以及研究区西北缘的阿拉善地区。
• 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。