淺色巖 的英文怎麼說
中文拼音 [jiānshǎiyán]
淺色巖
英文
leucocratic rock-
Normally tan to reddish sandstones are bleached.
黃褐色至淺紅色的砂巖通常是褪色的。Nature made this den, a cave undercutting bluff of beautiful orange - beige sandstone
這是個渾然天成的洞穴。山洞在一個淺桔色的砂巖峭壁之下。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
盆地基底由前寒武紀結晶基底和古生代褶皺基底組成，盆地蓋層則經歷了二疊紀的裂谷盆地、三疊紀?白堊紀的坳陷盆地和第三紀后的山間盆地的演化過程。盆地主要沉積了下二疊統巨厚火山巖、淺成侵入巖和凝灰巖；中二疊統蘆草溝組的暗色泥巖、泥灰巖、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、砂巖及灰色泥巖（下紅上灰） ；以及侏羅紀厚層深灰、灰色砂礫巖、砂巖、泥巖夾煤層。The artificial synthesis of hematite in granite can turn the color of common ligh - colored granite from grey or yellowish pink to red, which is of some significance in raising the utilization coefficient of common granite
通過在花崗巖中人工合成赤鐵礦，可使普通淺色（灰白、淺肉紅色）花崗巖改變為紅色，對提高普通花崗巖的利用率有一定意義。Submerged rocks are a pinkish-blue hue, while the open water tends to a desaturated blue.
淹沒在水中的巖石呈淺粉紅--藍色調，但地表水接近於不飽和的藍色。A. the granite is made up of quartz, feldspar and mica. it has the high degree of hardness, bearing abrasion, anti - shake, ant - press. its color primarily contain deep ash and shallow ash, emerald green, rose red and blue
花崗巖是由矽石英長石和雲母等細粒組成，具有高硬度耐磨抗震抗壓的特性。其?色主要有深灰和淺灰，翡翠綠玫瑰紅和蘭色。The cathodoluminescence ( cl ) analysis shows the quartz reflects an abundance of brown color, blue - purple, dark blue, dull color, and no cl color for quartz overgrowth, while feldspar shows light blue, yellow - green, yellow - brown, green and brown cl colors. the calcite reflects bright orange - yellow for non - ferroan calcite and dull orange - brown cl colors for ferroan calcite
陰極發光分析證實，砂巖中石英顆粒陰極發光顏色較深，主要位棕色、藍紫色、深藍色，石英加大變不發光；長石顆粒陰極發光顏色主要位淺藍色、黃綠色、綠色、棕黃色等；無鐵方解石陰極發光顏色為鮮艷桔黃色，鐵方解石陰極發光顏色為暗桔黃色。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「三砂夾兩灰」過渡為安多?茲格塘錯地層類型泥頁巖、泥灰巖，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，最後到深水盆地相的地層格架與沉積環境解釋模式。Edmond gazed very earnestly at the mass of rocks which gave out all the variety of twilight colors, from the brightest pink to the deepest blue ; and from time to time his cheeks flushed, his brow darkened, and a mist passed over his eyes
愛德蒙非常熱切地注視著那座山巖，山巖上正呈現著變化中的暮色，從最淺的粉紅到最深的暗藍，而熱血不住地往他臉上涌，額頭時而浮上陰雲，他的眼前時而呈現一片薄霧。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
蘆草溝組在盆地內部發育厚層暗色泥巖、泥晶灰巖、泥質白雲巖等，反映陸相淺一半深水沉積建造。Submerged rocks are a pinkish - blue hue, while the open water tends to a desaturated blue
淹沒在水中的巖石呈淺粉紅- -藍色調，但地表水接近於不飽和的藍色。S saw a dim and bluish light, which, as well as the air, entered, not merely by the aperture he had just formed, but by the interstices and crevices of the rock which were visible from without, and through which he could distinguish the blue sky and the waving branches of the evergreen oaks, and the tendrils of the creepers that grew from the rocks
，唐太斯本來以為洞里一定很黑暗，空氣中一定帶著濃重的腐臭味，但到了裏面，他卻看到一片淺藍色的昏暗的光線，這種光線，象空氣一樣，並非只是從他剛才挖開的洞口那兒射來的，是從巖石的裂縫里穿進來。這些在洞外是看不到的，但到了洞里，卻可以透過它們看到那蔚藍的天空，看到那些長在石縫里的常春藤，卷須蔓和野草的枝葉。Light gray, light yellow gray carbonate rock, clastic rock, a little amount mudstone with the gypsum rock in suonahu formation, regarding carbonate rock as principle
嗩吶湖組主要發育淺灰色、淺黃灰色碳酸鹽巖、碎屑巖，少量泥巖和石膏巖沉積，以碳酸鹽巖為主。The results show that there are many sedimentary facies in cretaceous of study area, such as alluvial fan with disorderly deposits, river with positive cycle, delta with middling maturity of petro composition and texture, and coastal and shallow lake sub - facies with deposits of thin multilateral mottle sand and shale
結果表明，研究區白堊系主要發育的沉積相類型有：雜亂堆積的沖積扇相；縱向上呈粒度向上變細的河流相；中等成分成熟度和結構成熟度的三角洲相；雜色砂泥巖呈薄互層沉積的濱淺湖亞相。分享友人