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Home > chinese-english > "wudaoliang" in English

English translation for "wudaoliang"

青海伍道梁
五道梁


Related Translations:
Example Sentences:
1.Therefore , the thesis thinks wudaoliang group and suonahu formation are the outcome of the miocene epoch
因此,论文认为五道梁群和唢呐湖组都是中新世时期的产物。
2.It is suggested that these anomalies are of radium nature having spot - form and deep - sourced features and are closely associated with wudaoliang fault
认为该航放异常系镭异常,具有点源、深源性质,与五道梁断裂密切相关。
3.Wudaoliang group is grayish - white , yellow - grey , dark - grey ash rock , which interbeded with the conglomerate , sandstone , a little amount mudstone , oil shale with unconsolidated sand mud rock
五道梁群以灰白色、灰黄色灰岩为主,含有砾岩、砂岩,夹有少量泥岩、油页岩和未固结砂泥沉积。
4.The lacustrine carbonate rocks occur on a wide range of scales in the palaogene and neogene strata in the hoh xil basin , qinghai , and constitute an important part of the miocene wudaoliang group sediments
摘要湖相碳酸盐岩在可可西里盆地的古、新近纪地层中分布广泛,更是中新统五道梁群沉积的主要组成部分。
5.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。
6.This paper emphatically analyses the distribution of airborne radiocactive anomalies in wudaoliang area , eastern chaidam basin , as well as the nature of these anomalies , locations , uranium and radium contents and uranium - radium equilibrium in anomalous areas
摘要本文著重分析了柴达木盆地东部五道梁地区航放异常的展布特徵、异常性质、产出位置,异常区铀、镭含量及铀镭平衡状态。
7.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。
8.The lacustrine carbonate rocks in the wudaoliang group consist of boundstone ( stromatolite ) , micritic limestone , grainstone and micritic dolostone which were laid down in the shallow - water to bathyal , high - salinity and enclosed to semi - enclosed lake systems
五道梁群湖相碳酸盐岩分为生物粘结灰岩(叠层石) 、泥晶灰岩、颗粒灰岩与泥晶白云岩四大类,反映出沉积环境为一个具有浅水半深水、高盐度、半封闭封闭特点的综合湖泊系统。
9.The volcanic rock age and the age of the qiangtang formation determined the wudaoliang group between 20 - 5ma , discovering a flood of spore and pollen with ostracods fossils ( regard eucypris as principle ) , which are miocene epoches typical numerator , therefore wudaoliang group accumulate in miocene epoch is doubtless ; 9 - 2ma are the age of the suonahu formation based on the data of the esr , which were characteristic of later period in miocene epoch - pliocene epoch , spore and pollen with fossil all were miocene epoch period
由火山岩和覆于其上的羌塘组的年龄限定五道梁群的沉积时间为20 - 5ma ,五道梁群中发现大量的孢粉和介形虫化石(以eucypris为主) ,分析认为它们都是中新世时期的典型分子,因此五道梁群的沉积时间为中新世是无疑的;唢呐湖组的esr测年数据范围为9 - 2ma ,代表中新世晚期?上新世时期,孢粉和化石都具有中新世时期的特征。
10.Dividing the sedimentary facies as a delta - lacustrine facies according to wudaoliang group sedimentary rock facies and its combination , regarding lacustrine facies as principle ; the northern qiangtang suonahu formation sedimentary facies was divided for fluvial facies and the lacustrine facies , regarding lacustrine facies as principle
根据五道梁群沉积岩相特征及其组合,将五道梁沉积相划分为扇三角洲- -湖泊相,以湖泊相为主。羌北盆地唢呐湖组沉积相划分为河流相和湖泊相,以湖泊相为主。
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