助手标题  
全文文献 工具书 数字 学术定义 翻译助手 学术趋势 更多
查询帮助
意见反馈
   new zealand 的翻译结果: 查询用时:0.013秒
图标索引 在分类学科中查询
所有学科
外科学
眼科与耳鼻咽喉科
生物医学工程
农业经济
教育理论与教育管理
地球物理学
林业
地质学
高等教育
更多类别查询

图标索引 历史查询
 

new zealand     
相关语句
  新西兰
     A PRELIMINARY STUDY OF EARTHQUAKE SWARMS IN RELATON TO MAJOR EARTHQUAKES (M≥7.0) IN NEW ZEALAND
     新西兰震群活动与大地震(M≥7.0)关系初探
短句来源
     GENECOLOGICAL DIFFERENTIATION OF THE INDIGENOUS SHRUB LEPTOSPERMUM SCOPARIUM (MYRTACEAE) IN NEW ZEALAND
     新西兰木本植物Leptospermum scoparium(Myrtaceae)的遗传生态学分化(英文)
短句来源
     ECOLOGY OF LEPTOSPERMUM SCOPARIUM IN NEW ZEALAND
     新西兰植物Leptospermum scoparium的生态学研究(英文)
短句来源
     Base Isolated Structures in New Zealand
     新西兰的基底隔震结构
短句来源
     GENERAL BIOMARKER CHARACTERISTICS OF CRUDE OILS FROM NEW ZEALAND
     新西兰原油生物标记化合物的一般特征
短句来源
更多       
  只新西兰
     Methods:180 New Zealand rabbits were used,and the Brodmann's 1,2,3,4,5,6,7,23,24 areas and partial 32,50 areas of the animal's cerebral cortex were excised.
     方法:用180只新西兰家兔,切除其大脑皮层Brodmann氏1、2、3、4、5、6、7、23、24以及部分32及50区。
短句来源
     Methods In 20 New Zealand white rabbits, 20 cartilage explants were taken from the knee joints in each rabbit, the size of which was 4 mm×4 mm×4 mm.
     方法20只新西兰兔,于膝关节切取20个4mm×4mm×4mm软骨块、25个2mm×2mm×2mm小软骨块、25个2mm×2mm滑膜片和25个2mm×2mm骨膜块。
短句来源
     Methods Forty New Zealand white rabbits were divided into two groups randomly:the control group(n=20)and the irradiation group(n=20).
     方法40只新西兰白兔随机分为对照组(n=20)和照射组(n=20)。
短句来源
     Methods The experimental model of 15 mm radial segmental defect was produced in 30 New Zealand white rabbits that were divided into group A and B according to transplant materials.
     方法选择30只新西兰白兔,制作15mm长的双侧桡骨节段性骨缺损模型,实验根据植入不同材料分为A、B组,A组分为A1组和A2组,A1组于动物左侧桡骨缺损区植入组织工程骨,A2组于右侧植入单纯材料。
短句来源
     Methods 6 New Zealand white rabbits were inoculated bilaterally with 1×105 PFU HSV-I McKrea strain.
     方法6只新西兰白兔双眼接种1×105PFU单纯疱疹病毒I型(HSV-I)McKrea株。
短句来源
更多       
  新西兰的
     Early onset neonatal meningitis in Australia and New Zealand, 1992- 2002
     1992—2002年澳大利亚和新西兰的新生儿早发性脑膜炎
短句来源
     Methods The New Zealand rabbits were exposed to 2 g/m 3 ( n =10) and 4 g/m 3 ( n =10) of TCE 4 h/d,4 d/week for 5 weeks by an inhalation chamber.
     方法 用浓度为 2、4g/m3 TCE分别对新西兰的白兔进行吸入式染毒 ,每日连续 4h ,每周 4d ,共 5周。
短句来源
     An Analysis on the Adaptation of New Chinese Immigrants in Australia and New Zealand
     华人新移民在澳大利亚、新西兰的生存适应分析
短句来源
     minutum isolated from Taiwan is very different from those of the species(LAC27 or 181NT strain) isolated from Western European, but similar with the sequence of the strain(Anakoha bay isolate) isolated from New Zealand.
     分离于我国台湾的微小亚历山大藻(A. minutum)在遗传序列信息上与分离自新西兰的藻株(Anakoha bay isolate)相似,而与分离自欧洲的藻株(LAC27 或181NT)相差较大。
短句来源
     Comparison of Iodine Stabilized He-Ne Laser Between China and New Zealand
     中国与新西兰的碘稳频氦氖激光器的比对
短句来源
更多       
  新西兰大
     Methods Craniocerebral gunshot injury model was established in 30 New Zealand white rabbits, which were subsequently exposed to environment of normal temperature (at 22.0±0.5 ℃ with relative humidity of 50%) or HHE at 39.0±0.5 ℃ with relative humidity of 80%-85% for 10 min, 30 min, 1 h, 1.5 h, and 2 h groups, respectively, with 5 rabbits in each group.
     方法采用高温高湿颅脑枪伤模型,新西兰大白兔30只,随机分成常温[(22.0±0.5)℃、RH50%]对照组,高温高湿[(39.0±0.5)℃、RH80%~85%]枪伤后受热10和30min,1h、1.5h、2h组,每组5只。
短句来源
     Methods Twenty-four hours after left anterior descending coronary ligation, New Zealand White rabbits were randomized to four groups: V group (valsartan 10mg kg-1 d-1), E group (enalapril 5mg kg-1 d-1), C group (control group) and S group (Sham group).
     方法冠状动脉左前降支结扎后24小时的新西兰大白兔随机分为3组:V组(valsartan 10mg·kg~(-1)·d~(-1)),E组(enalapril 5mg·kg~(-1)·d~(-1)),和C组(心梗对照组,Control group)。
短句来源
     [Methods] 30 adult New Zealand rabbits, weighed from 2. 8 - 3. 5 kg,were used in this experiment.
     【方法】成年新西兰大白兔30只,体质量2.8~3.5 kg。
短句来源
     Methods Fifty-six female New Zealand white rabbits were randomly divided into 4 groups:sham group,LVH group,KN-92 group and KN-93 group.
     方法雌性新西兰大白兔随机分为4组:假手术组(sham组)、心肌肥厚组(LVH组)、心肌肥厚+KN-93组(KN-93组)、心肌肥厚+KN-92组(KN-92组),每组14只。
短句来源
     Forty-eight New Zealand rabbits were made 1.2 cm bilateral radius defect models and divided into 4 groups averagely at random: group A(left:PRP/MSCs/β-tricalcium phosphate(β-TCP), right: MSCs/β-TCP), group B (left:auto-radius, right: PRP/MSCs/β-TCP);
     取48只1岁左右新西兰大白兔建立双侧桡骨1.2cm骨缺损模型,根据缺损中植入材料的不同随机分为4组,每组12只。 A组左侧PRP/MSCs/β-磷酸三钙(β-tricalciumphosphate,β-TCP),右侧MSCs/β-TCP;
短句来源
更多       

 

查询“new zealand”译词为其他词的双语例句

     

    查询“new zealand”译词为用户自定义的双语例句

        我想查看译文中含有:的双语例句
    例句
    为了更好的帮助您理解掌握查询词或其译词在地道英语中的实际用法,我们为您准备了出自英文原文的大量英语例句,供您参考。
      new zealand
    In order to demonstrate effects at different latitudes, the cases of high-latitude (Alaska), mid-latitude (Central Italy), and low-latitude (New Zealand) earthquakes were considered.
          
    Vertical Distribution of Pelagic Ostracods (Ostracoda, Halocyprinidae) in the Australian-New Zealand Sector of the Southern Ocea
          
    Samples of plankton from the Australian-New Zealand sector of the Southern Ocean have been examined.
          
    Latitudinal Distribution of Pelagic Ostracods (Ostracoda, Halocyprinidae) in the Australian-New Zealand Sector of the Southern O
          
    The latitudinal distribution of ostracods between the Subtropical Convergence and Antarctic Divergence has been studied from the example of materials from the Australian-New Zealand sector of the Southern Ocean.
          
    更多          


    Ⅰ. General SKETCH The Cenozoic basalt lavas are widely distributed along the coastal regionand its adjacent districts in eastern China. They form either widespread plateausor scattered mesa-like hills; and, in some places, the volcanic craters are stilladmirably preserved to-day. These basalt sheets were erupted extensively in lateTertiary and early Quaternary times. They belong to the multiple-vent basalts,but not the plateau basalt in the type of eruption. In this paper are given the results of a petrochemical...

    Ⅰ. General SKETCH The Cenozoic basalt lavas are widely distributed along the coastal regionand its adjacent districts in eastern China. They form either widespread plateausor scattered mesa-like hills; and, in some places, the volcanic craters are stilladmirably preserved to-day. These basalt sheets were erupted extensively in lateTertiary and early Quaternary times. They belong to the multiple-vent basalts,but not the plateau basalt in the type of eruption. In this paper are given the results of a petrochemical study of the Ceno-zoic basalt in eastern China. Geological and petrographical studies of the basaltsare not described in detail. Judging from the chemical compositions, the mostoutstanding characteristic feature of the most basaltic rocks is the richness inalkalis, especially in K_2O, also the undersaturation in silica, and, therfore,the most of the basalts distinctly belong to the alkaline rock suite. Such chemicalcharacters are closely related to modal compositions. The general petrogra-phical characters of the basalt may be now as well described. In North Chinaand South Manchuria most basalts are trachy basalt and its allied types, andoccasional nepheline basalt. The constituent minerals of these basalt are cha-racterized by the presence of anorthoclase, potash-adesine, plagioclase, titanaugite,as well as by the abundance of olivine. In South China the main basalt is olivinebasalt, consisting of olivine, augite, and plagioclase as usual. At some placesthe basalt may be slightly silica saturated that the occasional presence of hyper-thene and quartz (xenocryst) is noteworthy. In North Manchuria the dominant basalt is leucite basalt, containing leucite and olivine as phenocryst and groundmass constituent. Xenocryst of quartz and feldspar grains are sometimes present.In Taiwan Province, basalt of Kuanyinshan volcano is of the tholeiite type,but, in some other districts, the alkaline basalt with feldspathoidal constituentalso occurs. In view of the above-mentioned facts, the petrographical difference seemsto be matched by the differences of the major tectonic forms of China. Thesefacts may be tabulated below: Geographical region Tectonic forms Basalt type 1. North Manchuria Granitized region in Varisclde Leucite basalt 2. North China & South Precambrian Sino-Korean Trachybasalt Manchuria massive 3. South China Huanan platform in Yenshanide Olivine basalt 4. Taiwan Himalayide Tholeiite basalt Ⅱ. Regional INVESTIGATION In Table 1 the chemical analyses of the Cenozoic volcanic rocks in easternChina published up to 1951 were collected, of which 74 analyses are basalticrocks. The available analyses of every basalt sheet are taken an average to re-present the regional composition of the basaltic rocks. The localities of the basaltsheets where the analyzed chemical data are referable are shown in Figure 1.In all, 21 localities of basalt are investigated. The average chemical compositionsof each basalt locality, together with the normative minerals, Niggli's valuesand Zavarickij's numbers are given in Tables 2 A and 2 B respectively (localnos. in Table 2 correspond to the numerous in circle in Figure 1). For theconvenience of comparison, the average chemical composition of some standardbasalts (after S. R. Nockolds, 1954), some alkaline basalt in New Zealand (afterW. N. Benson, 1944) and Uganda (after A. Holmes, 1937), and the world's ba-salts, together with the normative minerals, Niggli's values and Zavarickij'snumbers of our calculation, are selected and given in Tables 3A, 3B, 7A, 7Brespectively. As mentioned above, the chemical composition of eastern China basalt ischaracterized by the high content of alkalies, and especially the K_2O. This cha-racter is definitely revealed by the normative feldspar, which is given in Table2 A and graphically shown in Figure 2. From this graphical representation,it is recognized that the normative feldspar becomes increasingly enriched ormolecular from South China to North Manchuria. Although the projected points appear to be scattered, a trend of clustering of the normative feldspars in accor-dance with its geographical distribution is apparent upon close inspection. Inthe normative pyroxene diagram, Figure 3, it is shown that most basalts of easternChina are rich in Wo molecular, falling near the Di-Hd line; On the otherhand, those of Kuanyinshan basalts of Taiwan Province are poor in Wo andcluster in the central part of the Di-Hd-Fs-En field. Therefore, that the easternChina basalt, excluding that of Kuanyinshan, belong to the alkaline rock suiteis justified. The comparison diagrams of qz, al-alk, C-(al-alk) and K-mg ofNiggli's values, based on the data given in Tables 2 B, 3 B, and 7 B, are gra-phically shown in Figs. 4, 5, 6 and 7 respectively. As will be seen from thesefigures, in general, the qz and al-alk of Niggli's value are lower, but C-(al-alk) and K-mg are higher than those of some common basalts. Fig. 8 isZavorickij's petrochemical vector diagram, from which the petrochemical cha-racters of high alkaline property in eastern China basalts are clearly justified. Ⅲ. Serial COMPARISON For ascertaining and understanding the general chemical characters, theCenozoic eastern China basalt and its differentiated associations are divided,based on the SiO_2 content, into 5 chemical types, the average composition ofwhich is given in Table 5A. As the chemical composition of Kuanyinshanvolcanic rocks in Taiwan Province shows a distinct calc-alkaline affinity, it is,therefore, dealt with the same procedure as well. The average chemical compo-sition of the volcanic rocks is given in Table 5 B. Since the Cenozoic basalt ineastern China covers the region adjacent to the Circum-Japan Sea and the Ja-panese Archipelagoes which are well known by the occurrence of alkaline andcalc-alkaline rock suite respectively. The serial variation in the chemical com-position of eastern China volcanic rocks is examinated in comparing them withthose of the Circum-Japan Sea and the Japanese volcanic rocks. The data usedfor the Circum-Japan Sea and Japanese rocks, which are given in Tables 6 A and6 B, are based on Tomita's and Yamada's calculated results respectively. Zavaric-kij's number of the same rocks, based on Zavarickij's data, is given in Table6 C. Following various petrochemical methods, some graphic diagrams are cons-tructed in order to express the chemical characters of the rock series of easternChina more definitely. The difference in chemical composition as comparedwith the Circum-Japan Sea alkaline rock suite is shown in the normal varia-tion diagram Figure 9. Other petrochemical indices (proposed by Peacock, Hol- mes and Tomita respectively) obtained are summarized below: Ⅰ Ⅱ Ⅲ Ⅳ alkali-lime index (Fig. 10) 65.5 59.0 63.0 52.0 alkali-alumina index (Fig. 11) -- -- 67.8 63.3 Ol-Q index (Fig. 12) 20.0 43.0 72.5 76.5 Ne-Hy index (Fig. 13) -- -- 55.0 59.9 Di-C index (Fig. 14) 46.5 46.5 -- -- Ⅰ. Japanese volcanic rocks; Ⅱ. Taiwan volcanic rocks; Ⅲ. Circum-Japan Sea alkaline suite; Ⅳ. eastern China volcanic rocks.From these graphical solutions in Figs. 10-14, it may be justified that thevolcanic rocks in eastern Asia have increasingly enriched the alkali contentfrom the Japanese Archipelagoes to the mainland of China. Figure 15 is avariation diagram of the normative feldspar of the eastern China series, incomparison with that of the Circum-Japan Sea region, the Japanese Archipela-goes and New Zealand. As will be seen from the diagram, the variation of thenormative feldspar of eastern China rock series is quite discriminative. Notonly is it richer in or molecular, but the positions of point N and O (corres-pond to the respective Ol-Q and Ne-Hy indices as shown in Figs. 12 and 13)of the eastern China series are also in a later course than the others. Figure 16is a paragenetic diagram of the normative plagioclase and pyroxlene of theeastern China series. In the variation diagram of the normative pyroxene, Fig.17, the distinct difference in the course of variation between the alkaline andcalc-alkaline series is clearly revealed. In this connection, the directon of varia-tion in the normative pyroxene of the alkaline series differs from that of thecalc-alkaline series. It is also notable that the range of variation in the easternChina series is smaller, due to the presence of higher Wo molecular in bothbasic and acidic types, as compared with that of the Circum-Japan Sea series.Figure 18 is Zavarickij's petrochemical vector diagram of the eastern Chinaseries compared with that of Circum-Japan Sea and Japanese series. It may be acomplemental diagram of the serial comparison diagram of eastern Asia volcanicrock series, prepared by Zavarickij (cf. A. N. Zavarickij's Introduction to Petro-chemistry of Igneous Rocks, 1950, Fig. 61, p. 205, in Russian). The distinctdifference of these rock series may be clearly observed in the graphical solution.In Table 7 A is given the average chemical composition of eastern China basalt,together with the composition of basaltic rocks of the world (including olvinebasalt and Toleiite, Ocean basalt and Continent basalt) for comparison. Theeastern China average is very similar to the average composition of the olivine- basalt of the Circum-Japan Sea region (based on Tomita, 1935, and recalculatedby the writer), while it differed more or less from that of any of the world'sbasalts by the high content of alkali and especially K_20. This character isdefinitely revealed by the normative feldspar and pyroxene, which are graphi-cally shown in Figs. 19 and 21 respectively. Figure 20 is Zavarickij's petroche-mical diagram of the world's basalt. As shown in these diagrams, it suggests atransitional relation rather than a sharp cleft in the petrochemical charactersof the world's basalts. There are no distinct types of basalt magma but rathera continuous series from silica saturated (tholeiitic) to silica-undersaturated(olivine-basalt) rock, although the chemical distinction may be too subtle to beread directly from chemical analyses. Ⅳ. ORIGINAL Basalt Magma The original magma of eastern China basalt belongs to the olivine basaltmagma type. In this discussion it is assumed that the primary olivine basaltmagma is melted from a crust of peridotitic crystalline rock in the upper partof the sima layer. Olivine basalt magma may be modified by the gain of alimited amount of silica and some alkalies to produce a derived melt, whichappears to coincide with the thole

    ~~

    The second paper describes a period of high b value which preceded some large and intermediate earthquakes in some areas of China,New-Zealand,the United States of America and Venezuela.The dura- tion of the period and its regional distribution are related with the magnitudes of the main shocks.The duration of high h value may result from variations in the media in the seismo-genic regions which are under a contain kind of stress within a period prior to a large shock,and this may he of some significance...

    The second paper describes a period of high b value which preceded some large and intermediate earthquakes in some areas of China,New-Zealand,the United States of America and Venezuela.The dura- tion of the period and its regional distribution are related with the magnitudes of the main shocks.The duration of high h value may result from variations in the media in the seismo-genic regions which are under a contain kind of stress within a period prior to a large shock,and this may he of some significance for intermediate estimations of forthcoming major earthquakes.

    介绍了中国、新西兰、美国和委内瑞拉地区的一些大、中地震前出现一个高 b 值时期,该时期的长短及其区域分布范围与主震震级有关。高 b 值时期可能是大震前某一时期处在某一应力状态下的孕震区介质性质的变化引起的,这对估计未来大震的中期趋势有一定意义。

    In this paper, the spatial-temporal characteristics of earthquake swarms from 1955 to March, 1981, which may be related to the occurrence of major earthquakes (M≥7.0) in New Zealand are investigated. The preliminary results are as follows : 1 ) Several years before the major earthquakes, the swarm activity increased in a wide area, the frequency of swarm was about 2 times more than the normal level. The space pattern of the swarm distribution was constrained by the tectonic conditions. 2 ) Several months...

    In this paper, the spatial-temporal characteristics of earthquake swarms from 1955 to March, 1981, which may be related to the occurrence of major earthquakes (M≥7.0) in New Zealand are investigated. The preliminary results are as follows : 1 ) Several years before the major earthquakes, the swarm activity increased in a wide area, the frequency of swarm was about 2 times more than the normal level. The space pattern of the swarm distribution was constrained by the tectonic conditions. 2 ) Several months before the occurrence of the major earthqakes (M≥7.0), swarms with similar characteristics occurred correspondingly both in the Milford Sound region and the Hawke's Bay. 3 )Since the Milford Sound earthquake (M≥7.0) of 1976 up to the present day, no obvious anomalies in the swarm activities in New Zealand have been detected.

    本文研究了1955年至1981年3月新西兰地区(36°S—47°S,166°E—179°E)震群活动的时空分布特征,及其与大地震(M≥7.0)发生的关系。初步结果表明:(1)大地震发生前数年,大范围震群活动增强,其频度约为一般水平的两倍,空间分布受构造条件的制约;(2)震前数月,在米尔福桑德(Milford Sound)地区和霍克斯(Hawkes)湾地区相呼应地出现类似频震群活动;(3)1976年米尔福桑德 M=7.0地震后至今,新西兰震群活动的度、强度和空间展布范围,未见有明显异常。

     
    << 更多相关文摘    
    图标索引 相关查询

     


     
    CNKI小工具
    在英文学术搜索中查有关new zealand的内容
    在知识搜索中查有关new zealand的内容
    在数字搜索中查有关new zealand的内容
    在概念知识元中查有关new zealand的内容
    在学术趋势中查有关new zealand的内容
     
     

    CNKI主页设CNKI翻译助手为主页 | 收藏CNKI翻译助手 | 广告服务 | 英文学术搜索
    版权图标  2008 CNKI-中国知网
    京ICP证040431号 互联网出版许可证 新出网证(京)字008号
    北京市公安局海淀分局 备案号:110 1081725
    版权图标 2008中国知网(cnki) 中国学术期刊(光盘版)电子杂志社