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vertical sense
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  垂直方向
     On vertical sense of tree structure,81.9% availability indeterminate shoots were set upper and middle of canopy where distance 100~200 cm from earth surface.
     在垂直方向上,有效结果母枝主要集中在树冠上部和中部距地面100~200 cm处,层内有效结果母枝数占81.9%;
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  “vertical sense”译为未确定词的双语例句
     In contrast, the basement in the footwall moved in a vertical sense in response to unloading, and therefore records decompression of 0. 4-0. 6 GPa and uplift.
     相反,拆离带下盘的基底岩石则表现为与卸载有关的垂向运动,因而记录了0.4—0.6GPa的减压抬升。
短句来源
     All kinds of micro-components and sulphide occurrence varied through vertical sense in different coal strata whic h is the reflection of coal concentration.
     各类显微组分含量乃至硫化物产状等沿垂向不同煤层呈规律性变化,这是聚煤环境变化的反映。
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     A good understanding of the works' style,appreciation of works of music,singing techniques,the vertical sense of the concord as well as the thoughts in the works——these are all the important problems that a singer shoued solve,whether he or she is on the concert stage or in a casual performance.
     无论是在音乐会的舞台上还是在平时的歌唱表演中,对音乐作品风格的理解、音乐鉴赏力、旋律线条的歌唱技巧、和声的纵向感以及作品的思想性等,都是歌唱者要解决的重要内容。
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  相似匹配句对
     vertical hemilaryngectomy;
     喉垂直部分切除术;
短句来源
     Vertical Limit
     垂直极限
短句来源
     Sense of Humor
     美国人的幽默
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     sense of law;
     培养学生的法律与社会公德意识;
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     Current gain β of vertical transistor in BiCMOS technology and SPC in a broad sense
     BiCMOS工艺中纵向晶体管β和广义SPC
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  vertical sense
Freedom of expression is becoming a reality, in both a hor izontal and a vertical sense.
      
For structures that are very uniform in a vertical sense, the two procedures give very similar results.
      
Consequently, we believe that the anomalies we observe are well resolved in the entire mantle, in a horizontal as well as vertical sense.
      


The tectonic and P-T histories of both TTG gneiss and khondalite series in the Datong-Huaian area are different but interrelated to each other. A low-angle high strain zone lying between the two rock series is characterized by ductile shearing in a normal sense and noncoaxial deformation , showing a tectonic contact between them. Structural, textural and stratigraphic data indicate that the terrain was affected by two tectono-thermal cycles (C1 and C2) and two corresponding granulite facies events (M1 and M2)...

The tectonic and P-T histories of both TTG gneiss and khondalite series in the Datong-Huaian area are different but interrelated to each other. A low-angle high strain zone lying between the two rock series is characterized by ductile shearing in a normal sense and noncoaxial deformation , showing a tectonic contact between them. Structural, textural and stratigraphic data indicate that the terrain was affected by two tectono-thermal cycles (C1 and C2) and two corresponding granulite facies events (M1 and M2) about 2500 and 1800 Ma ago. The major structures in the terrain were formed during M1, C1 is manifested by regional crustal compression and thickening in the early stage and subsequent extension and decoupling. In C1 the peak metamor-phic conditions were 1. 2-1. 4 GPa and 800-900 C ; while for the allochthonous cover sedi- ments the values were about 0. 8 GPa and 800 C and there were developed bedding-parallel foliation and large amounts of S-type granites. The earlier structures in basement and allochthonous cover are products of M1 metamorphic event at different crustal levels. Juxtaposition of basement and cover along a detachment zone occurred at the late stage of C1/M1. The cover sequence in the hanging wall of the detachment was displaced in a lateral sense and syn-D3 structure records cooling rather than decompression. In contrast, the basement in the footwall moved in a vertical sense in response to unloading, and therefore records decompression of 0. 4-0. 6 GPa and uplift. During C2/ M2, peak conditions of about 0. 4-0. 6 GPa and 650-700 C were reached. This period witnessed the development of discrete, left-lateral strike-slip zones that transect both basement and cover, accompanied by uplift. The low-angle detachment and deduced P-T paths imply that there occurred extensional collapse in the process of isostatic adjustment following crustal thickening.

大同—怀安地区TTG片麻岩和孔兹岩系早期具有互不相同的、但又彼此相关的构造和温压历史。它们之间的低角度高应变带以正韧性剪切和非共轴变形为特征,体现了构造接触的性质。构造和岩石学数据表明,该地体至少在2.5Ga和1.8Ga前后分别受到两个麻粒岩相变质事件(M_1,M_2)的影响,其主要的构造是在M_1事件中形成的。早期构造-热事件表现为区域地壳挤压加厚和随后发生的伸展拆离。其峰期变质温度达800—900℃,压力达1.2-1.4GPa;在异地变质沉积岩中,早期构造-热事件的峰值温度大致为800℃,压力为0.8GPa左右,形成了与岩性层平行的面理,井发育大量S型花岗岩。基底和异地盖层中的早期构造代表M_1变质事件在不同地壳层次上的产物。两者沿大型拆离带的位移调整发生在M_1的晚期(D_3):拆离带上盘的盖层岩石表现为侧向位移滑脱,其中D_3期构造记录了比减压更为显著的冷却过程;相反,拆离带下盘的基底岩石则表现为与卸载有关的垂向运动,因而记录了0.4—0.6GPa的减压抬升。M_2期间发育了同时切过基底和盖层的北东向走滑带,同时伴随着某些抬升。M_2的峰期压力为0.4—0.6GPa,温度为650-700℃。上述低角度...

大同—怀安地区TTG片麻岩和孔兹岩系早期具有互不相同的、但又彼此相关的构造和温压历史。它们之间的低角度高应变带以正韧性剪切和非共轴变形为特征,体现了构造接触的性质。构造和岩石学数据表明,该地体至少在2.5Ga和1.8Ga前后分别受到两个麻粒岩相变质事件(M_1,M_2)的影响,其主要的构造是在M_1事件中形成的。早期构造-热事件表现为区域地壳挤压加厚和随后发生的伸展拆离。其峰期变质温度达800—900℃,压力达1.2-1.4GPa;在异地变质沉积岩中,早期构造-热事件的峰值温度大致为800℃,压力为0.8GPa左右,形成了与岩性层平行的面理,井发育大量S型花岗岩。基底和异地盖层中的早期构造代表M_1变质事件在不同地壳层次上的产物。两者沿大型拆离带的位移调整发生在M_1的晚期(D_3):拆离带上盘的盖层岩石表现为侧向位移滑脱,其中D_3期构造记录了比减压更为显著的冷却过程;相反,拆离带下盘的基底岩石则表现为与卸载有关的垂向运动,因而记录了0.4—0.6GPa的减压抬升。M_2期间发育了同时切过基底和盖层的北东向走滑带,同时伴随着某些抬升。M_2的峰期压力为0.4—0.6GPa,温度为650-700℃。上述低角度拆离带和所得到的P-T轨迹,意味着紧随地壳加厚之后的均衡调整过程发生了伸展拆离。

The tectonic evolution of the North China region roughly experienced five stages, i. e. the continental nucleus and basement formation stage, the Mesoproterozoic and Neoproterozoic aulacogen development stage, the Palaeozoic stahle platform development stage with orogenic movement on its north and south margins, the middle and late Mesozoic transitional stage from the Eurasian tectonic domain to marginal-Pacific tectonic domain, and the Cenozoic marginal-Pacific tectonic domain development stage. Regional tectonic...

The tectonic evolution of the North China region roughly experienced five stages, i. e. the continental nucleus and basement formation stage, the Mesoproterozoic and Neoproterozoic aulacogen development stage, the Palaeozoic stahle platform development stage with orogenic movement on its north and south margins, the middle and late Mesozoic transitional stage from the Eurasian tectonic domain to marginal-Pacific tectonic domain, and the Cenozoic marginal-Pacific tectonic domain development stage. Regional tectonic evolution had obvious controlling effects on the petroleum formation in the Bohai Bay basin and even the North China region. The framework of alternately arranged uplifts and depressions determines the targets of exploration for Palaeozoic petroleum and Meso-Cenozoic buried-hill petroleum accumulations. The NE-trend-ing deep faults control the development and distribution of Meso-Cenozoic volcanic rocks in the Bohai Bay basin; so the exploration of volcanic rock oil-gas pools is a very important in the future. As the tectonic evolution in the Bohai Bay basin progressed stage by stage, the distribution of oil-gas pools show: a three layer oil-bearing model in the vertical sense. Tectonic migration determines that the distribution of oil-gas pools have a certain regularity in plan in the Bohai Bay basin.

华北地区的构造演化大致经历5个阶段,即陆核及基底形成阶段;中、新元古代裂陷槽发育阶段;古生代稳定地台发育阶段及其南北缘的造山作用;中生代中后期欧亚构造域与滨太平洋构造域过渡期;新生代滨太平洋构造域大发展时期。区域构造演化对渤海湾乃至华北地区油气的形成和分布具明显控制作用,主要表现在:中生代隆坳相间格局决定了古生代油气勘探的方向,是勘探新生古储潜山油气藏的主要地区;渤海湾盆地火山岩油气藏勘探也是今后一段时期内重要的勘探领域之一;渤海湾裂陷盆地构造演化的阶段性使得油气藏的分布在垂向上具有“三层楼式”的含油模式;构造迁移性导致渤海湾盆地油气藏在平面上的分布具有一定的规律性。

Liaocheng coal area has 6 sheets which belong to Tai yu an formation, and 2 sheets which belong to Shanxi formation. Organic micro-compo sitions are majorly composed of vitrinite, also including niertinite, semi-vitri nite, exinoid group; inorganic micro-compositions are majorly composed of clay g roup, others are carbonate and sulphide group. All kinds of micro-components and sulphide occurrence varied through vertical sense in different coal strata whic h is the reflection of coal concentration.

聊城煤矿区属太原组的可采煤6层,属山西组的可采煤2层。各煤层煤岩有机显微组成以镜质组为主,次为惰性组、半镜质组、壳质组;无机显微组成以粘土组为主,次为碳酸盐组和硫化物组。各类显微组分含量乃至硫化物产状等沿垂向不同煤层呈规律性变化,这是聚煤环境变化的反映。

 
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