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block collision
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  “block collision”译为未确定词的双语例句
     Based on detailed study, it was suggest that in the last stage of Wutai orogeny, the block collision between Fuping and Hengshan caused the deep-level strlke-sliping and folding which in turn created a tectonic condition for formation and rising of magma and provided the space for its emplacment at last.
     研究认为:五台运动末期,阜平古陆与恒山古陆发生的碰撞,造成了深部走滑作用和活动带中地层(五台群)褶皱,为岩浆的形成、演化提供了构造环境,并为其定位提供了空间。
短句来源
     The Zhongdian arc is located at the southern end of Yidun island arc in the Sanjing tectono magmatic zone. Its evolution involved ocean crust subduction orogeny (210~235 Ma), continental block collision (80~88 Ma) and convergence orogenics of continental margins (28 Ma).
     中甸弧位于西南三江构造火成岩带义敦岛弧的南端 ,它的演化经历了洋壳俯冲 ( 2 10~ 2 3 5Ma)、陆陆碰撞 ( 80~ 88Ma)和陆内汇聚 ( 2 8Ma)三大造山作用。
短句来源
     I type biotite granites and related Mo W deposits of quartz vein type and altered granite type were formed during continental block collision orogenics.
     在碰撞造山作用中形成了与后造山黑云母花岗岩和与之有关的蚀变花岗岩型、石英脉型钨 钼矿床。
短句来源
  相似匹配句对
     Block and Z.
     B lock和Z.
短句来源
     Collision and Integration
     冲撞与整合
短句来源
     Collision and Choice
     碰撞与选择
短句来源
     Gypsum block
     石膏砌块
短句来源
     Subduction and collision was both normal and oblique, depending on the direction of block movements and on the configurations of individual blocks.
     “斜向碰撞型山链”与走滑断裂的形成、规模及其运动学直接相关。
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  block collision
The algorithm is based on the two-block collision differential path of MD5 that was presented by Wang et al.
      
In this paper, we present a fast attack algorithm to find two-block collision of hash function MD5.
      


The trisected scale terrace is the overall characteristic of Chinese relief. It is observable with reference to relative Gravity anomaly and earth crust thicknes in China, and dependent on the epicontinental spreading, the land block collision and the isostasy of the earth crust.

“三级阶梯”是中国地形的总体特征,它与我国的重力异常、地壳厚度变化有着明显的对应关系,是地壳均衡、陆缘扩张、陆块碰撞的必然结果.

West China has been pieced with the following Palaeozoic-Triassicplates and terranes, the Siberian Plate, the Kazakhstanian Plate, theTarim-Sinokorean Plate composed of the Tarim, Qaidam, Alxa, Helan-Liupan and North China terranes, the South China-Southeast Asia Platemade of the Changning-Menglian, Shuangjiang-Lancang, Changdu andYangtze terranes in the west part of the plate, the Zangbei(North Tibet)-Dianxi (West Yunnan) Microplate containing the Karakorum, Lhasa,Gangmacuo, Tengchong and Baoshan terranes and...

West China has been pieced with the following Palaeozoic-Triassicplates and terranes, the Siberian Plate, the Kazakhstanian Plate, theTarim-Sinokorean Plate composed of the Tarim, Qaidam, Alxa, Helan-Liupan and North China terranes, the South China-Southeast Asia Platemade of the Changning-Menglian, Shuangjiang-Lancang, Changdu andYangtze terranes in the west part of the plate, the Zangbei(North Tibet)-Dianxi (West Yunnan) Microplate containing the Karakorum, Lhasa,Gangmacuo, Tengchong and Baoshan terranes and the Indian Plate. Great Meso-Cenozoic continental spreading basins of West China areconsiderably developmental. They can be divided into inland spreadingbasins including the Junggar, Tarim and Qaidam basins and back-arcspreading basins containing the Bayan Har, Tanggula, Changdu, Lanping-Simao and Zangbei basins. The basins are closely related with the sub-duction mechanism of the adjacent ocean. Since Late Permian the main geological events, which occurred inChina, comprise three times of continental block collisions including sub-duction of the allied ocean plate in company with the development ofcontinental spreading basins and a time of interplate continental crustsubduction. The Cathaysian Collision Period from Late Permian to LateTriassic, in which the Tarim-Sinokorean Plate and the South China-Southeast Asia Plate split from Pacifica came into the collision withthe Angara old land, forming the Eurasian Plate and accompanied bythe transformation from the Paleotethys Ocean into the Mesotethys Ocean,take the general layout of the Meso-Cenozoic tectonic evolusion of China.The Zangbei Collision Period from Late Triassic to Early Cretaceous: ischaracterized by the subduction of the Mesotethys Ocean Plate, the clo- sure of the Mesotethys Ocean and the collision of the Zangbei-DianxiMicroplate divided from Gondwana with the Eurasian Plate. The Zangnan(South Tibet) Collision Period from Late Triassic to Middle Eocene,in which the Indian Plate is connected with the Eurasian Plate, is markedby the closure of the Newtethys Ocean and an intensive orogenic movementshowing an extensive unconformity. Since Late Eocene the north part ofthe Indian Plate subduces northwards under the Eurasian Plate by meansof a wide zone of imbricate thrust faults, exhibiting a kind of interplatecontinental crust subduction. There are two principal types of the Meso-Cenozoic orogeny of China:I. A Continental Spreading Basin Orogeny and 2.An Ocean SpreadingBasin Orogeny divided into two subtypes, a Continental Collision Orogenyincluding ocean plate subduction and continental block collision and anInterplate Continental Crust Subduction Orogeny. The thickness of thecontinental crust of China is very uneven because of secondary thickeningand thinning. There are two thickening ways of the continental crust:1. A lmbricate Thrust Thickening, in which the crust is thickened by aseries of imbricate thrust faults overlapped thrustedly each other, distribu-ting along continental crust subduction zones of intraplate andinterplate; 2. A Transmission-squeeze Thickening, in which the crust ma-terial is eroded and carried to mountain roots at margins of spreadingbasins by the secondary mantle convections. The crust is thinned with twoways: 1. A Pull-Extension Thinning, in which the crust is thinned bymeans of normal fault systems; 2. A Transmission Spreading Thinning,in which the crust is thinned by the secondary mantle convectioas trans-miting basin materials to margins of spreading basins.

中国西部中新生代大型大陆扩张盆地相当发育,可分为内陆扩张盆地和弧后扩张盆地。这两种盆地的形成和演化与相邻大洋板块俯冲机制密切相关。晚二叠世以来,中国发生过三次与大洋板块俯冲相关的陆块碰撞和一次显著的板间陆壳俯冲。中国中新生代造山运动主要是由大陆扩张盆地和大洋扩张盆地的扩张作用引起的,因此存在两种造山运动的基本类型。中国中新生代大陆壳厚度颇不均匀,增厚是通过叠冲和传递挤压方式实现的;减薄是凭借拉伸和传递扩张方式进行的。

Hefei basin and the fold area of Huainan and Huaibei as parts of the North China block underwent multi-lager detachment and decoupling of both the cover and the basement during the Mesozoic Orogeny. Thrust and nappe structures developed in sinian though paleozoic strata meet in opposite dicections. The basement is characterized by ductile overlap thrusts or subduction faults and displaced in opposite directions. A model of intra continental basement shortening in the process of continental block collision...

Hefei basin and the fold area of Huainan and Huaibei as parts of the North China block underwent multi-lager detachment and decoupling of both the cover and the basement during the Mesozoic Orogeny. Thrust and nappe structures developed in sinian though paleozoic strata meet in opposite dicections. The basement is characterized by ductile overlap thrusts or subduction faults and displaced in opposite directions. A model of intra continental basement shortening in the process of continental block collision has been presented in the present paper.,

华北地合皖中复式褶皱与拗陷盆地是中生代陆壳多层次拆离滑脱造山运动之产物。北侧发育推覆、滑覆构造,对接于凤-定山区;南为合肥拗陷。结晶基底断块沿先存铲型伸展断层,作反向继承性仰冲或俯冲,使陆壳加积缩短。本文提出了一个在大陆地块碰撞下,以多层次构造拆离为背景的陆壳缩短模式。

 
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