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western hubei
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  鄂西
     Phosphorite can be divided into three industrial mineral beds, i.e. Ph_1,Ph_2,Ph_3,and phosphorus bearing bed Ph_4 in Doushantuo Formation of Western Hubei.
     鄂西陡山沱组磷块岩可以划分为三个工业矿层Ph_1,Ph_2,Ph_3和一个含磷层Ph_4,具有全区对比意义的有Ph_1,Ph_2和Ph_4。
短句来源
     In this paper, focal mechanisms of 23 moderate and small earthquakes (Ms = 2.0-5.1) in the area of the western Hubei occurring during 1972-1985 are analysed.
     本文分析了1972—1985年鄂西地区23个中小地震(M_s=2.0—5.1)震源机制解。
短句来源
     A Study on the Gravitational Geological Hazards in Western Hubei
     鄂西重力地质灾害的研究
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     Application of Integrated Geophysics in Residual Basin of Western Hubei
     鄂西残留盆地综合地球物理应用研究
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     Quantitaive classification of the main types of forest vegetation in the reservoir area of Shiziguan power station in western Hubei
     鄂西狮子关电站库区主要森林植被类型的数量分类
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  湖北西部
     There are 9 genere, 54 species and 6 varieties in Anthemideae (Compositae)in Western Hubei, of which medicine plants 14, perfume 7, tannin 1, flower 2, vegetable 2, fodder 4, and toxic 5.
     湖北西部菊科春黄菊族植物有9属,54种,6变种,其中药用植物14种,香料植物7种,鞣料植物1种,花卉2种,蔬菜2种,饲料4种,有毒植物5种。
短句来源
     There are 21 genere,54 species, 1 subspecies, 7 varieties and 1forma in western Hubei(Inuleae Helintheae Helenieaa), of which 2 species and 1 varieties are reported the new distribution in Hubei, 2 species in Shennonjia. These plants have many applications,of which medicine 30,petrfume 8,flower 7, fodder 2, vegetable 2,oil-bearing crops 2,fibre 1,tannic material 1 and plant coloring matter 1.
     湖北西部菊科植物(旋复花族。向日葵族。堆心菊族)共有21属,54种,1亚种,7变种,1变型,其中2种,1变种为湖北省地理分布新纪录,2种为神农架地理分布新纪录,这些菊科植物有许多用途,其中药用植物30种,香料植物8种,花卉植物7种,饲料,蔬菜和油料作物各2种,纤维,鞣料和植物色素植物各1种。
短句来源
     There are 13genera, 53 species, 4 subspecies and 5 varieties of compositae (Senecioeeae and Calenduleae)in western Hubei, of which 2 species are reported the new distriburion in Shennongjia.
     湖北西部菊科千里光族和金盏花族植物共有13属,53种,4亚种,5变种,其中2种为神农架地理分布新记录。
短句来源
     THE COMPOSITAE OF WESTERN HUBEI(Ⅰ)
     湖北西部菊科植物(Ⅰ)——斑鸠菊族、泽兰族、紫菀族
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     MIDDLE TRIASSIC MARINE OSTRACODS FROM WESTERN HUBEI
     湖北西部海相中三叠世介形类
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  “western hubei”译为未确定词的双语例句
     The section is located near Wangjiawan village, 42km north of Yichang city (western Hubei, China), at 30°58′56″N and 111°25′10″E on the east flank of the Huangling Anticline.
     该剖面位于中国湖北省宜昌市以北42km处的王家湾村,经纬度为30°58′56″N、111°25′10″E。
短句来源
     FURTHER OBSERVATIONS ON ARCHAEOPTERIS MACILENTA LESQUEREUX FROM WESTERN HUBEI
     鄂西马西伦达古羊齿(Archaeopteris macilenta Lesquereux)的再观察
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     NEW DISCOVERIES OF LOWER CAMBRIAN CRUSTACEAN FOSSILS FROM WESTERN HUBEI
     鄂西下寒武统甲壳类化石新发现
短句来源
     The result was to set up the reaction system of RAPD and ISSR fitting for analyzing the resources of pummelo in western Hubei.
     建立了一套适合于分析柚种质资源的RAPD和ISSR反应体系。
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     The Characteristics and Distribution Pattern of Karst Water in Western Hubei
     鄂西南岩溶水的基本特征及分布规律
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  western hubei
A dendrochronological technique was used to investigate canopy recruitment of beech (Fagus engleriana Seem.) trees in western Hubei Province of Central China by identifying growth releases through gap formation.
      
Geochemistry of the Yutangba Se deposit in western Hubei, China
      
The western Hubei mountainous area includes the Wudang, Jingshan, Daba and Wushan Mountains.
      


The internal structure of Pleurodium Wang,1955(Braehiopoda)found from theupper part of Lojoping Formation,Dazhongba,Yichang district,western Hubei ishere dealt with in detail.Its ventral valve is characterized by spondylium curvedstrongly far into the dorsal valve and very short median septum.Both outer andinner brachial plates of the dorsal valve rather finely thin and short,only 1—2 mm.in length;brachial processes thintabulated,projecting laterally and crossing in anobtuse angle with the inner brachial...

The internal structure of Pleurodium Wang,1955(Braehiopoda)found from theupper part of Lojoping Formation,Dazhongba,Yichang district,western Hubei ishere dealt with in detail.Its ventral valve is characterized by spondylium curvedstrongly far into the dorsal valve and very short median septum.Both outer andinner brachial plates of the dorsal valve rather finely thin and short,only 1—2 mm.in length;brachial processes thintabulated,projecting laterally and crossing in anobtuse angle with the inner brachial plates.The valves,as a whole are composedmainly of fibrous layer,but devoid of prismatic layer.It may be concluded that incomparison with other relevant families,subfamilies and genera,and taking into ac-count its inner structure and outer morphological feature,the present writers tend toassign Pleurodium to Family Virgianidae,with Pleuodiinae,as new subfamily.To thebest knowledge of the present writers,Pleurodium is distributed restrictively in Sou-thwest China and is believed to be the early Late Llandoverian in age.It is worthmentioning that Pleurodium,known to occur in association with Stricklandia andPentamerus,is therefore of important significance in establishing ecological communityposition.

本文详细研究了产自湖北宜昌志留系罗惹坪组的腕足化石Pleurodium tenuiplicatum(Grabau)的内部构造,讨论它和有关类别的关系,确定Pleurodium 的分类地位;建立肋房贝新亚科(Pleurodiinae,subfam.nov.),归于枝线贝科;并阐述Pleurodium 的地质地理分布和地层意义,指出其时代为晚兰多维列世早期。

The Silurian strata well developed in the Yichang area,Western Hubei,wereformerly divided into three formations,in ascending order,Lungmachi,Lojoping andShamao(C.Y.Hsieh and Y.T.Chao,1925;T.H.Yin,1949;A.T.Mu,1959),andhave recently been revised into five units:(see Table 1).Among these units,theLungmachi formation(ss),is very rich in graptolites,whereas in the others grapto-lites are rather rare.Based on the study of graptolites,all the formations except theShamao(ss)are considered to be of Lower Silurian...

The Silurian strata well developed in the Yichang area,Western Hubei,wereformerly divided into three formations,in ascending order,Lungmachi,Lojoping andShamao(C.Y.Hsieh and Y.T.Chao,1925;T.H.Yin,1949;A.T.Mu,1959),andhave recently been revised into five units:(see Table 1).Among these units,theLungmachi formation(ss),is very rich in graptolites,whereas in the others grapto-lites are rather rare.Based on the study of graptolites,all the formations except theShamao(ss)are considered to be of Lower Silurian age.The material dealt with in the present paper contains 50 species and subspeciesbelonging to 17 genera and 1 subgenus,of which,1 genus,1 subgenus and 34 speciesand subspecies are new.According to the different characters,the virgula of Petalolithus from WesternHubei may be divided into three types:(1)Expansive type:virgula expanded gradually,with only one vane.(see Text.2,fig.1)(2)Zonary type:virgula with three vanes of uniform width.(see Text.2,fig.4)(3)Broomy type:virgula is multibrachiate.(see Text.2,fig.2)The new genus and new subgenus may be diagnosed as follows:Genus Dischidograptus Ni gen.nov.Type species:Petalolithus mirabilis Mu et al.Biserial,axonophorous graptoloid,rhabdosome scandent proximally and dividingdistally into 2 uniserial reclined stipes,forming“Y”-shape;thecae long,with gentleventral curvature,overlap considerable;virgula dividing repeatedly to from complexbuoyancy.(see Text.Ⅱ,fig.3).Based on the distal character of the rhabdosome,Petalolithus ovatus scopaecu-larus Schauer may be grouped in this new genus.Genus Rastrites Barrande,1850Subgenus R.(Lituigraptus)Ni subgen,nov.Type species:R.(Lituigraptus)glomeratus subgen,et sp.nov.Rhabdosome curved,thecae isolate,apertures of proximal thecae hooked,those ofdistal thecae broader,opening outward with long and paired apertural spines.According to the peculiar thecal character,Rastrites phleoides T■rnquist seems tobe a member of this subgenus.

本文着重研究湖北宜昌早志留世笔石的新材料,共描述18属50种,其中有一个新属和一个新亚属,34新种和新亚种,从而对本地区的志留系划分提供了依据,并对早志留世笔石带作了补充。在研究花瓣笔石(Petalolithus)特征和轴囊构造的基础上,认为Petalolithusmirabilis Mu et al.应独立成属,定名为分裂笔石(新属)(Dischidograptus gen.nov.)。根据笔石体胞管口部特征,在耙笔石属(Rastrites)中,建立一新亚属,取名为喇叭笔石(新亚属)Rastrites(Lituigraptus)subgen.nov.。

The study of organic reef has important significance in the exploration of oil and gas fields. Huangnitang organic reef was found by us in Huangnitang Commune of Lichuan, Hubei in 1977. Its horizon belongs to the First Submember of the Second member, Upper permian Changxing Formation. The reef appears at the flanks and northeast plunging end of Huangnitang Anticline, which spreads from northeast to southwest. It is 15 km in visible length, 45 km in breadth and 134.3 m thick. The Limestones of the reef...

The study of organic reef has important significance in the exploration of oil and gas fields. Huangnitang organic reef was found by us in Huangnitang Commune of Lichuan, Hubei in 1977. Its horizon belongs to the First Submember of the Second member, Upper permian Changxing Formation. The reef appears at the flanks and northeast plunging end of Huangnitang Anticline, which spreads from northeast to southwest. It is 15 km in visible length, 45 km in breadth and 134.3 m thick. The Limestones of the reef are pure in quality, light in colour, not uniform in texture and structure, and are obviously paleogeomorphological high in topography. Besides this, it is principally characterized by being rich in reef——building organisms in situ growth (central reef area). The principal reef—building organisms are sponges, bryozoas, corals, stromatoporas and algae and so on. Among them, the sponges and algae take advantageous position in quantity.The reef—core and fore—reef can be seen camparatively completely.According to the wave—resistant ways which are shown by the texture of the rocks, the rocks of the reef—core subfacies are divided into bafflestone, bound—framestone, and boundstone. This district is abundant in the bafflestone with baffletexture. The so—called baffletexture is that the micritic matrix grew everywhere between the sponges and the other reef—building organisms. It shows that the deposites resisted the wave through the reef—biulding organisms baffling the micritic matrix. The bound—framestone with bound—frametexture is the most mature rock of reef—core in evolution. The frameworks or its miniature models are composed of the finger and massive reef—building organisms They formed unshakable skeletons through the binding—action of the coated bluegreen algae. and the interskeletons are filled with sparry calcites. The boundstones provide bound—frameworks which are composed of coated bluegreen forms and some bound organisms, and the interframeworks are also filled with sparry calcites.The forereef subfacies are composed of calcirudites and bioclastic limestones.According to the microfacies festure in perpendicular sections of Huangnitang organic reef, the development history of the reef growth may be divided into 4 stages: primary, principal, inconsecutive and decadent.Solution porosites and intercrystal porosites are the principal pore space of the reservoir. Recently, some gas beds have already been found by drilling in western Hubei. It proves that the prospect of the reefal gas field is quite bright.

生物礁的研究对油气田的勘探具有重要意义。黄泥塘生物礁是我们1977年在鄂西利川县黄泥塘公社一带实测二迭系剖面时发现的。其层位属上二迭统长兴组第二段第一亚段(P_1C_1~2)。出露于黄泥塘背斜两翼和北东倾没端,呈北东——南西向展布。已见长度15公里,宽4.5公里,最大厚度134.3米。礁相段岩石除具有质纯、色浅、结构构造不均匀以及在产状上呈明显的古地貌凸起等特点外,富含原地生长的造礁生物(指礁核)是其主要特征。主要的造礁生物有海绵、苔藓虫、珊瑚、层孔虫和藻类等。其中海绵和包壳状兰绿藻在数量上是最重要的。黄泥塘生物礁的礁核和礁前出露较完整。礁核亚相岩石根据其结构特征所反映的抗波方式,可分为障积岩、粘结~骨架岩和粘结岩三种。障积岩是本区出露最多的一种礁核亚相岩石,具障积式结构特征,亦即在原地生长的海绵等造礁生物之间,广泛发育灰泥杂基,反映了沉积物是通过造礁生物对灰泥杂基的障碍作用而抗波的。粘结~骨架岩是发育最成熟的礁核岩石,具有粘结~骨架式结构特征,亦即指状、块状造礁生物组成骨架或骨架雏形,经包覆生长的包壳状兰绿藻的粘结而形成坚固的骨架,架间充填亮晶方解石。粘结岩由包壳(或迭层)状兰绿藻和少量被缠绕的生物组成粘结...

生物礁的研究对油气田的勘探具有重要意义。黄泥塘生物礁是我们1977年在鄂西利川县黄泥塘公社一带实测二迭系剖面时发现的。其层位属上二迭统长兴组第二段第一亚段(P_1C_1~2)。出露于黄泥塘背斜两翼和北东倾没端,呈北东——南西向展布。已见长度15公里,宽4.5公里,最大厚度134.3米。礁相段岩石除具有质纯、色浅、结构构造不均匀以及在产状上呈明显的古地貌凸起等特点外,富含原地生长的造礁生物(指礁核)是其主要特征。主要的造礁生物有海绵、苔藓虫、珊瑚、层孔虫和藻类等。其中海绵和包壳状兰绿藻在数量上是最重要的。黄泥塘生物礁的礁核和礁前出露较完整。礁核亚相岩石根据其结构特征所反映的抗波方式,可分为障积岩、粘结~骨架岩和粘结岩三种。障积岩是本区出露最多的一种礁核亚相岩石,具障积式结构特征,亦即在原地生长的海绵等造礁生物之间,广泛发育灰泥杂基,反映了沉积物是通过造礁生物对灰泥杂基的障碍作用而抗波的。粘结~骨架岩是发育最成熟的礁核岩石,具有粘结~骨架式结构特征,亦即指状、块状造礁生物组成骨架或骨架雏形,经包覆生长的包壳状兰绿藻的粘结而形成坚固的骨架,架间充填亮晶方解石。粘结岩由包壳(或迭层)状兰绿藻和少量被缠绕的生物组成粘结式格架,架间充填亮晶方解石。礁前亚相岩石为砾屑灰岩和生物屑灰岩。根据黄泥塘生物礁各剖面纵向微相特征,可将礁的发育史分为成礁初期;主要成礁期;断续成礁期和退化期等四个时期。溶孔和晶间孔是礁相岩石的主要储集空间,最近鄂西某地巳从与黄泥塘生物礁的同时期礁相岩石中钻开了较高产的气层,从而进一步证实了本期生物礁的良好含气性能,展示出礁性气田勘探的良好前景。

 
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