泥灰岩的英文

音标：[ níhuīyán ] 发音:

"泥灰岩"怎么读用"泥灰岩"造句

英文翻译手机版

boglime
chalky ciay
chalky clay
malm
mare
marl stone
marlite
marlstone
muddy limestone

"泥灰；泥灰岩" 英文翻译 : marl
"泥灰土；泥灰岩；灰泥" 英文翻译 : marl
"白泥灰岩" 英文翻译 : acendrada; chalk marl
"白雪泥灰岩" 英文翻译 : dolomite-marl
"白云泥灰岩" 英文翻译 : dolomite-marl
"白垩泥灰岩" 英文翻译 : chalk marl
"贝壳泥灰岩" 英文翻译 : shell marl
"茶绿泥灰岩" 英文翻译 : tea-green marl
"叠锥泥灰岩" 英文翻译 : tutenmergel
"钙质泥灰岩" 英文翻译 : calcareous marl(clay)
"海成泥灰岩" 英文翻译 : marine marl
"含镁泥灰岩" 英文翻译 : dolomitic marl
"含铜泥灰岩" 英文翻译 : kupfermergel
"红泥灰岩" 英文翻译 : red marls
"湖泥灰岩" 英文翻译 : lake marl
"灰质泥灰岩" 英文翻译 : calcareous marl; calcareousmarl
"介壳泥灰岩" 英文翻译 : falun; shell marl
"轮藻泥灰岩" 英文翻译 : chara limestone; chara marl
"泥灰岩的" 英文翻译 : marlaceous; marly
"泥灰岩坑" 英文翻译 : marlpit
"泥灰岩相" 英文翻译 : marlaceous face; marlaceousface; marly facies
"泥灰岩砖" 英文翻译 : gault brick; marl brick
"泥质泥灰岩" 英文翻译 : argillaceous marl
"青泥灰岩" 英文翻译 : blue marl
"泥灰岩捆吊床结用细绳扎紧" 英文翻译 : marl
"泥灰土之一种" 英文翻译 : marlstone

例句与用法

Especially in shuanghu area and amdo 114 station , the sedimentary rocks is organic - rich , mostly consist of black shales , marls and mudstones
尤其是双湖地区和安多114道班岩性特殊，为一套富含有机碳沉积，主要为黑色页岩、泥灰岩和泥岩。
The thesis analysises the typical model profile and the special rock profile of wudaoliang group of miocene epoch in hoh xil basin . and be used the biocalcarenite with the marl rock take the marker bed of wudaoliang group
论文对可可西里盆地中新世五道梁群的典型剖面和特殊岩性剖面进行了分析，并以泥灰岩和生物碎屑灰岩作为五道梁群的标志层。
The microfacies of carbonate rock of the wudaoliang group in hoh xil basin is divided for marl lithofacies , micrite facies , micrite ( spar ) scraps ash lithofacies , grain scraps micrite facies , dolimite rock lithofacies , and the stromatolite ash lithofacies
可可西里盆地五道梁群碳酸盐岩微相类型主要为泥灰岩相、泥晶灰岩相、泥(亮)晶粒屑灰岩相、粒屑泥晶灰岩相、白云岩相、叠层石灰岩相、核形石灰岩相等7种微相。
The northern qiangtang basin suonahu formation microfacies of carbonate rock is divided for the intraclast ash lithofacies , biological detritus ash lithofacies , oncolite limestone lithofacies , contain the calcium and alga ash lithofacies , marl lithofacies and pure microlite limestone lithofacies
羌北盆地唢呐湖组碳酸盐岩微相为内碎屑灰岩相、生物碎屑灰岩相、核形石灰岩相、含膏藻灰岩相、泥灰岩相和纯微晶灰岩相等6种微相。
Through the analysis of the stratigraphy and sedimentary facies of the research areas , the description model between the stratigraphic framework and deposite environment can be set up firstly by the transition from the " three horizons sandstone with two intercalated limestone horizons ' mn yanshiping area to shale and marl in amdo - zigetang co , and to oil shale in bilong co , then by the transition of the shallow water platform facies to the deep water continental shelf , slope , and to the deep water basin
通过对研究区地层和沉积相分析，建立起一个从北向南由雁石坪地层类型“三砂夹两灰”过渡为安多?兹格塘错地层类型泥页岩、泥灰岩，最后到比洛错地层类型黑色油页岩，由浅水台地相过渡到深水陆棚、斜坡，最后到深水盆地相的地层格架与沉积环境解释模式。
5 . the fractures of marlite , sandstone , faults and the disconformity between sha san member and sha er member are three main conduit systems . for this low maturity of the oil kitchen , the fractures of marlite that coexist with source rock might as well be an important bridge to link oil kitchen and reservoir
5 、通过对德南洼陷输导体空间分布及物性特征分析，揭示并论证了本区特殊的输导层主要是与源岩共生的泥灰岩、泥质白云岩及白云岩中的裂缝系统，为进一步寻找有关油气藏指出方向。
Three sets of source rocks had been formed juring the steady sinking of the basin . the first source rock , being clay and calcium clay stone in tiemulike formation of permian was formed in deep lake environment ; the second source rock , being clay stone in xiaoquangou group of middle to upper triassic was formed in the offshore and the shallow lake environment ; and the third source rock , being coal beds in badaowan formation of lower jurassic was formed in the lake - swamp environment . the first one is the most potential , since it has the biggest thickness , the highest organic matter abundance , high maturity and the highest hydrogen generating capacity
在盆地稳定沉降时期，相应地形成三套烃源岩，即上二叠统铁木里克组( p _ ( 2t ) )深湖、半深湖相泥岩、泥灰岩；中上三叠统小泉沟群( t _ ( 2 - 3xq ) )滨浅湖相泥岩及下侏罗统八道湾组( j _ ( 1b ) )湖沼相煤系地层。
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。