灰泥盆 的英文怎麼說

中文拼音 [huīpén]
灰泥盆 英文
plaster pot
  • : Ⅰ名詞1 (物質燃燒后剩下的粉末狀的東西) ash 2 (塵土; 某些粉末狀的東西) dust 3 (特指石灰) lime...
  • : 泥名詞1 (含水的半固體狀的土) mud; mire 2 (像泥的東西) any paste like matter; mashed vegetable...
  • : 1. (盛東西或洗東西用的器具) basin; tub; pot 2. (姓氏) a surname
  1. The microfacies characteristic of carbonate rock of suonahu formation in cuoqinin basin constitutes with the marl lithofacies, the intraclast ash lithofacies, biological detritus ash lithofacies

    措勤地嗩吶湖組碳酸鹽巖微相由內碎屑巖相、生物碎屑巖相和巖相組成。
  2. 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

    論文對可可西里地中新世五道梁群的典型剖面和特殊巖性剖面進行了分析,並以巖和生物碎屑巖作為五道梁群的標志層。
  3. 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

    可可西里地五道梁群碳酸鹽巖微相類型主要為巖相、巖相、(亮)晶粒屑巖相、粒屑巖相、白雲巖相、疊層石巖相、核形石巖相等7種微相。
  4. 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

    羌北地嗩吶湖組碳酸鹽巖微相為內碎屑巖相、生物碎屑巖相、核形石巖相、含膏藻巖相、巖相和純微晶巖相等6種微相。
  5. 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

    地基底由前寒武紀結晶基底和古生代褶皺基底組成,地蓋層則經歷了二疊紀的裂谷地、三疊紀?白堊紀的坳陷地和第三紀后的山間地的演化過程。地主要沉積了下二疊統巨厚火山巖、淺成侵入巖和凝巖;中二疊統蘆草溝組的暗色巖、巖、白雲質巖石以及條湖組的巨厚層火山巖、侵入巖;三疊系雜色砂礫巖、砂巖及巖(下紅上) ;以及侏羅紀厚層深色砂礫巖、砂巖、巖夾煤層。
  6. 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

    地穩定沉降時期,相應地形成三套烴源巖,即上二疊統鐵木里克組( p _ ( 2t ) )深湖、半深湖相巖、巖;中上三疊統小泉溝群( t _ ( 2 - 3xq ) )濱淺湖相巖及下侏羅統八道灣組( j _ ( 1b ) )湖沼相煤系地層。
  7. Lithologically different rock sheets intertexturally superimposed with faults and folds of various styles. while, the southern belt is chiefly of devonian tuff, tuffaceous schist, marble relatively stable in strata and manifested by regional asymmetric fold easi - westward in axis, with well developed superimposed overthrust south - northward which controlled the whole structural framework in this area

    南帶以系凝巖、凝質片巖、大理巖為主,地層相對穩定,表現為軸向東西的區域性不對稱褶皺,廣泛分佈控制全區構造格局的南北向逆沖推覆的疊瓦式斷裂。
  8. According to the differences of sedimentary facies and environment, the source rock are divided into four types such as lime - mud reef in platform margin, platform inner sag, deep - water flat slope or continental shelf, abyssal basin, the lime - mud reef type is distributed in platform margin of upper ordovician, the remained three types are widely distributed in cambrian - ordovician system

    根據沉積相帶與沉積環境的不同,可將烴源巖劃分為在不同沉積環境中的4種類型烴源巖;臺地邊緣丘型烴源巖、臺地內凹陷型烴源巖、深水緩坡與陸棚型烴源巖、深海地型烴源巖。
  9. 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

    通過對研究區地層和沉積相分析,建立起一個從北向南由雁石坪地層類型「三砂夾兩」過渡為安多?茲格塘錯地層類型頁巖、巖,最後到比洛錯地層類型黑色油頁巖,由淺水臺地相過渡到深水陸棚、斜坡,最後到深水地相的地層格架與沉積環境解釋模式。
  10. Were found in the margin around the basin. lucaogou fm. was mainly composed of thick dark mudstone, micritic limestone, argillaceous dolomite, which reflected a shallow to fairly deep - lake sedimentary formation

    蘆草溝組在地內部發育厚層暗色巖、巖、質白雲巖等,反映陸相淺一半深水沉積建造。
  11. Carboniferous strata, more than 1000m in thick in the area of hexi corridor to bayan haot basin, is the coal measures of transitional phase, in which there are three kinds of hydrocarbon source rocks including dark mudstone, limestone, coal and carbonaceous mudstone

    摘要河西走廊至巴彥浩特地地區石炭紀地層厚逾千米,是一套海陸交互相含煤巖系,發育暗色巖、巖、煤層及碳質巖等3大類烴源巖。
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