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  active
    Symposium on Research Results in Seismic Risk and Earthquake Prediction in the Seismically Active Area of Tucuman, U. S. S. R
    土库曼地震活动区的地震危险性和预报研究成果报告会
短句来源
    CHARACTERISTICS OF THE ACTIVE TECTONICS AND MORPHOGENETIC MOVEMENTS IN CHINA
    中国活动构造与造貌运动的特征
短句来源
    FAULTING EVENTS OCCURRED IN YISHU FAULT ZONE IN THE PAST 40,000 YEARS——APPLICATION OF ~(14)C TECHNIQUE TO ACTIVE FAULT STUDY
    沂沭断裂带四万年来的新活动——~(14)C技术在活动断裂研究中的应用
短句来源
    A General Account of Studies on Moving Mechanism, Slip Rate and Earthquake Recurrence Rate of Some Active Rifts in China
    中国几条活动断裂的运动机制、滑动速率和地震重复性的研究概述
短句来源
    THE CHARACTERISTICS OF THE ACTIVE FAULTS IN THE 1668 GREAT EARTHQUAKE (M = 81/2)AREA, JUXIAN-TANCHENG,SHANDONG PROVINCE
    1668年山东莒县—郯城8 1/2级大震区的活动断裂特征
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  movement
    ANALYSIS ON GEOLOGICAL AGENTS CONTROLLING MOVEMENT OF THE ROCKBODIES
    控制岩体活动的地质因素分析
短句来源
    SIGNIFICANCE OF THE STUDY OF REPEATED MOVEMENT OF FAULTS
    断裂多期活动及其研究意义
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    Recent Tectonic Movement and Recent Crust Stress Field in Yuncheng Basin
    运城盆地的现今构造活动及现代地壳应力场的基本特征
短句来源
    Characteristics of Recent Crustal Deformation Movement in Shanxi Region
    山西地区近期地壳形变活动特征
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    Five phases of neotectonic movement took place along the Jiayuguan fault during the latest Pleistocene to Holocene,i. e. at 4.3-4.5,12.9-14.0,20.0-23.2,35.5-45 and 58.1 ka BP.
    晚更新世晚期~全新世存在5期明显的新构造活动,分别发生于距今稍大于4.3ka、稍大于12.9ka、20.0~23.2ka、35.5~45ka和稍大于58.1ka。
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  the active
    CHARACTERISTICS OF THE ACTIVE TECTONICS AND MORPHOGENETIC MOVEMENTS IN CHINA
    中国活动构造与造貌运动的特征
短句来源
    THE CHARACTERISTICS OF THE ACTIVE FAULTS IN THE 1668 GREAT EARTHQUAKE (M = 81/2)AREA, JUXIAN-TANCHENG,SHANDONG PROVINCE
    1668年山东莒县—郯城8 1/2级大震区的活动断裂特征
短句来源
    THE ACTIVE PATTERN OF SMALL EARTHQUAKES AND THE FEATURES OF FOCAL REGION STRESS FIELD BEFORE AND AFTER THE LINGWU EARTHQUAKE OF Ms5.5 ON AUG. 10, 1987
    1987年8月10日灵武5.5级地震前后小震活动图象及震区应力场特征
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    STUDY ON GRAVITY CHANGES ALONG THE ACTIVE FRACTURE BELTS IN BEIJING AREA
    北京地区活动断裂带上的重力变化的研究
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    GEOCHEMICAL CHARACTERISTICS OF GASES ALONG THE ACTIVE FAULT ZONES IN THE SOUTHERN ZHANGJIAKOU AREA
    张家口南部地区活动断裂带气体地球化学特征
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  “活动”译为未确定词的双语例句
    Middle Proterozoic Tectonic Morbile Belt and Mineralization in North Continental Margin of the North China Plateform
    华北板块北缘中元古代大陆边缘构造活动带及成矿
短句来源
    Structural Transformation and Strain Partitioning along the Northeast Boundary Belt of the Sichuan-Yunnan Block
    川滇块体北东边界活动构造带的构造转换与变形分解作用
短句来源
    TANGSHAN GREAT EARTHQUAKE AND ITS FORSHOCKS AND AFTERSHOCKS
    唐山大震及其前后的地震活动
短句来源
    THE FAULT FRAME CLASSIFICATION FOR GREAT EARTHQUAKES AND THE SEISMICITY CHARACTERISTICS BEFORE THE GREAT EARTHQUAKES
    大地震发震断裂格架分类与大震前的地震活动特征
短句来源
    PATTERN RECOGNITION OF SEISMICITY BEFORE STRONG EARTHQUAKES
    大震前地震活动的图象识别
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  active
The Design and Synthesis of a Novel, Orally Active, Selective ETA Antagonist
      
The pharmacokinetics of α- and β-diastereomers of Arteether, a well-known antimalarial drug and its active metabolite dihydroartemisinin (DHA) were studied in Sprague-Dawley rats, Rhesus monkeys and human volunteers.
      
The same compounds were studied using CoMFA for which the molecules were first aligned to a template molecule, which was most active in the series.
      
Among these compounds, 6-benzo[1,3]dioxol-5-yl-4-oxo-hex-5-enoic acid (3) was the most active one.
      
Only 15.33% of the cells was metabolically active at 200 μg/ml methanol extract while 23.57% of the cells was active at 200 μg/ml berberine.
      
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  movement
In this paper the secant methods are also improved by adding a dogleg typed movement which allows to overcome a phenomena similar to the Maratos effect.
      
The movement of interest rates becomes more important in pricing such long-dated options.
      
The results demonstrate that the actuator is characterized by a simple structure, large movement range, strong driving ability and high positioning resolution.
      
According to the movement in the images and the characters of spectrum, the motion compensation and raising coefficients of intensive interference area were used in this wavelet.
      
Here, the actuation mechanism of the sandwiched-configuration EWOD chips was carefully studied, and the movement of droplets was numerically analyzed by using the computational fluidic software, CFD-ACE+.
      
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  the active
The 'active' compounds, which reduced growth of cancer cells to ca.
      
The resulting data were analyzed and suitable models were developed after identification of the active ranges.
      
Resulting data were analyzed and suitable models were developed after identification of the active ranges.
      
The active site and crystal nucleus are formed due to the comprehensive effect of electricity, thermodynamics and chemistry.
      
The active power P and the reactive power Q are obtained through the PQ transformation of the stator currents.
      
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Various kinds of acid igneous rocks are found around the Kushan, to theeast of Foochow, Fukien. One earlier variety of the granites, provisionally termedas Kushan Granite, is coarser-grained, often flesh-colored, and biotite-bearing,similar in character to the most frequently seen and widely distributed graniteof whole Fukien; the other, the Kueichi Granite, often intruding into the firstnamed, is colored by different shades of grey, mostly, fine-grained, and mia-rolitie, containing minor amount of hornblende...

Various kinds of acid igneous rocks are found around the Kushan, to theeast of Foochow, Fukien. One earlier variety of the granites, provisionally termedas Kushan Granite, is coarser-grained, often flesh-colored, and biotite-bearing,similar in character to the most frequently seen and widely distributed graniteof whole Fukien; the other, the Kueichi Granite, often intruding into the firstnamed, is colored by different shades of grey, mostly, fine-grained, and mia-rolitie, containing minor amount of hornblende instead of biotite, yet sometimesvarying its texture to felsitic, porphyritic, or even to micro-graphic. In thecourse of weathering, the soils thus formed from these two granites, as well astheir corresponding surface vegetations are also evidently dissimilar. That the Kueichi granite was really intruding into the Kushan is evidencedby its ramifying apophyses in the latter, its broad marginal phase, its miaro- litie cavities elongated and lined parallel to the intrusive contact and the"sericitization front", so to show a convex curvature facing the Kushan Graniteside along their mutual contact. The prevalent strike of the contact of the granites conicides with thefracture and joint systems of the Kushan Granite, one set of which is N65°E,being also parallel to one of the major vertical joints of the Kueichi. This isprobably due to the prolonged fracturing during the formation of Pacificfolding zones of the Chekiang and Fukien coast, rendering the KueichiGranite intruding along the said fracture system yet itself subjected to the samemechanical stress. Rocks correlated to these two granites are found elsewhere in Fukien. Theymay also be comparable to the two granites of Sihwashan, S. Kiangsi, foundby C. S. Mo and his colleagues. The repeated intrusions of the Post-Jurassicgranites may allow to consider the possibility of repeated formations of theirgenetically related ores. The lead-zinc deposits of Yuntai and Lungyai areprobably related to the igneous activity of the Kueichi Granite.

经初步瞭解,福建鼓山分布着两种后侏罗纪花岗岩。这从岩石地面分布上的接触情况与显微镜下观察的岩石中组成成分的接触情况两方面得到证实的。从二者产生状态看来,彼此生成时间甚为接近,而同属於太平洋运动产物,分属早晚期活动。再根据前人各种地质文件,推论出福建各地普遍存在着相当於这两种侵入的花岗岩类岩石。因此,联系到福建后侏罗纪金属矿成矿作用的多次性可能。这在江西西华山已有发现。此后从多次性来研究后侏罗纪的炎成矿床的成矿作用,成为必要了。

In recent years, the geotectonic problem of China engages the attentionof many Chinese and Soviet geologists, but different opinions are confessed by different authors. After studying the structural characters of the fundamentalfloor and its later geological development, theauthor of this paper agrees withthe statement of the Soviet geologist, B. M. Синицын. In 1952 he pointed outthat the Chinese platform in eastern China, may bs divided into: (1) theSine-Korean platform; and (2) the Southern-Chinese platform,...

In recent years, the geotectonic problem of China engages the attentionof many Chinese and Soviet geologists, but different opinions are confessed by different authors. After studying the structural characters of the fundamentalfloor and its later geological development, theauthor of this paper agrees withthe statement of the Soviet geologist, B. M. Синицын. In 1952 he pointed outthat the Chinese platform in eastern China, may bs divided into: (1) theSine-Korean platform; and (2) the Southern-Chinese platform, consolidatedas a result of the Luliang movement. This Chinese platform especially in its southern part shows a very peculiarphenomenon as it is called "Activization" of the platform. During Sinian andPaleozoic, its sediments belonged to the pronounced epi-continental type, duringthe mesozoic the south-eastern part of the Southern-Chinese platform wasneither a stable shelf nor a geosyncline, but an intermediate type between them.Its characters were really not geosynclinal, but sometimes showed geosynclinalaffinities, as for instances, the immense granitic intrusions, the eruptions oflavas, and the rather strongly folded geosynclinal structures. These imply thelimited mobility or the incomplete consolidation of the underground. Accor-dingly, referred to the structural type of this region, P. Misch called it"Sinotype". Furthermore, in the Southern-Chinese platform, two strong "Activizingunits" are recognized as follows: 1) The Hunan-Kwangsi activizing andsubsiding region; 2) The Cathaysian activizing oldland. The "Activization"of these regions lasted for a long geological time. It began in Sinian, throughCaledonian, Variscian, Indo-Sinian, Yenshanian and even Himalayan. BeforeMesozoic, the Caledonian was the most intensive and widely distributed one.But as pointed out by A. H. Мазарович, the Caledonian of the Southern-Chineseplatform was merely a fold-belt within the platform. According to its geotectonic history, its character of sedimentation, itsregional metamorphism, its igneous activity and its geotectonic systems, suchas "Kwangsi ∈ system", "North-Kwangtung ∈ system", "Meso and Neo-Cathaysiansystem", and the "Nanling eastwest tectonic zone", it is the author's opinionthat the "Imtermediate type (Sinotype)" of the Southern-Chinese platform wasdeveloped gradually through a long "Activizing process". This "Sinotype" is anintermediate type between the stable shelf and the geosynclinal region.

作者同意B.M.西尼村的意见,认为中国地台是中国东部的一个大的构造单位,它是在吕梁运动后造成的。中国地台由两个主要部分构成,它的北部称中朝地台,南部称华南地台。中国地台有一很重要的特征,就是一个“活化”的地台。华南地台的东南部“活化”尤其强烈而显著,在中生代的太平洋运动时,差不多具有类似地槽的特征。但是它的“活化”是有悠久历史的,即开始於震旦纪,所以加里东运动给与很大的影响,但加里东运动只是地台内部的褶皱。地台“活化”直到中生代太平洋运动才得到高度发展,产生巨大的火成活动以及“中国式”的构造型式。新生代时地台还有中等强度的运动和火成活动。自第四纪冰期之后,地台仍在较弱的升降运动中。华南地台无论从沉积岩相、区域变质及火成活动,或从山字型、华夏式及南岭东西褶皱的构造体系等构造型式发育史的研究,都可以看到它的“活化”过程,在这过程里发育了“过渡类型”的构造形态,这都是不同放地槽或地台的构造形态的。本文是作为学习心得性质的初步尝试,文中不成熟和谬误之处尚多,希望得到大家的指正。如果能在集体的讨论和研究之下将我国大地构造研究清楚的话,这是作者所衷心期望的。

~~

本文在綜合研究宁鎮山脈象山羣岩层縐构造形态基本特征、分布規律和形成机理的基础上,专門論述了海西印支裡縐构造的基底断裂如何控制燕山盖层褶縐形成的具体表現方式,論証了燕山运动以块断运动为主的构造性貭,为进一步研究下揚子地区岩漿活动和成矿作用的空間分布規律提供了构造方面的依据。

 
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