单词 | 石灰岩 |
释义 | 〔oolite〕Rock, usually limestone, composed of oolites.岩石:岩石,通常指石灰岩,由鲕粒岩组成〔pisolite〕Rock, usually limestone, composed of pisoliths.豆石,豆岩:由豆石构成的岩石,常为石灰岩〔Wolds〕A range of chalk hills in northeast England along both banks of the Humber River.丘陵地:英格兰东北亨伯河两岸的一个石灰岩构成的山脉〔marble〕A metamorphic rock formed by alteration of limestone or dolomite, often irregularly colored by impurities, and used especially in architecture and sculpture.大理石:由石灰岩或白云岩变化而来的一种变质岩,常有不规则的杂质色块,专门用于建筑和雕塑〔karst〕after the Karst , a limestone plateau near Trieste 源自 喀斯特 ,德里雅斯德港附近一个石灰岩高地 〔limestone〕A common sedimentary rock consisting mostly of calcium carbonate, CaCO3, used as a building stone and in the manufacture of lime, carbon dioxide, and cement. 石灰岩:一种普通沉积岩,主要成分为碳酸钙,CaCO3,用于建筑,并用于制造石灰、二氧化碳和水泥 〔limestone〕limestone cliffs; limestone walls.石灰岩峭壁;石灰岩墙〔oolite〕A small round calcareous grain found, for example, in limestones.鲕粒岩:含有圆形小颗粒的石灰质岩石,如在石灰岩中〔sinkhole〕A natural depression in a land surface communicating with a subterranean passage, generally occurring in limestone regions and formed by solution or by collapse of a cavern roof.灰岩坑:与某一地下通道相联的陆地表面的自然下沉地区,通常出现在灰岩地区并且由石灰岩溶解成溶洞顶部下沉形成〔karst〕An area of irregular limestone in which erosion has produced fissures, sinkholes, underground streams, and caverns.喀斯特:由于腐蚀而产生裂隙,落水洞,潜流和洞穴的不规则的石灰岩地区〔nummulite〕A large, coin-shaped, fossil foraminifer of the genusNummulites, widely distributed in limestone formations from the Eocene Epoch to the Miocene Epoch of the Cenozoic. 货币虫:货币虫 体形大而呈硬币状,化石有孔的虫,从始新世到新生代的中新世广泛分布在石灰岩地层中 〔cenote〕A water-filled limestone sinkhole of the Yucatán.洞状陷穴:犹加敦地区有水的石灰岩竖洞〔rendzina〕A dark soil that develops under grass on limestone and chalk.黑色石灰土:在石灰岩和石灰上生长的草下形成的黑色土壤〔buhrstone〕A tough, silicified limestone formerly used to make millstones. It is typified by the presence of multiple cavities that originally housed fossilized shells.磨石,砂质多孔石灰岩:一种坚硬的,硅化石灰石,以前用来制作磨石。具有最初由化石化的贝壳而形成的多孔特征〔Eifel〕A hilly region of western Germany west of the Rhine River. The barren area has limestone moors and crater lakes.艾弗尔:位于德国西部的莱茵河西岸的丘陵地带,土地贫瘠,有石灰岩泥沼和火口湖〔Carmel〕A limestone ridge of northwest Israel extending about 24 km (15 mi) from the Plain of Esdraelon northwest to the Mediterranean Sea. It rises to approximately 546 m (1,790 ft).加尔默多山:以色列西北部一石灰岩山脉,从埃斯德赖隆平原向西北延伸24公里(15英里)至地中海。海拔约546米(1,790英尺)〔carbon〕Symbol C A naturally abundant nonmetallic element that occurs in many inorganic and in all organic compounds, exists freely as graphite and diamond and as a constituent of coal, limestone, and petroleum, and is capable of chemical self-bonding to form an enormous number of chemically, biologically, and commercially important molecules. Atomic number 6; atomic weight 12.01115; sublimation point above 3,500°C; boiling point 4,827°C; specific gravity of amorphous carbon 1.8 to 2.1, of diamond 3.15 to 3.53, of graphite 1.9 to 2.3; valence 2, 3, 4. See table at element 符号 C 碳:一种在自然界很丰富的非金属元素,存在于很多无机化合物和有机化合物中,以石墨和金刚石的形式以及作为煤,石灰岩和石油的一种成份大量存在,能在化学上自我结合而形成大量化学上,生物上和商业上重要的分子,原子序数6;原子量12.01115;升华点高于3,500°C;沸点4,827°C;非结晶质碳的比重为1.8至2.1,钻石的比重为3.15至3.53,石墨的比重为1.9至2.3;化合价为2,3,4 参见 element |
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