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assimilate with
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     RS monitoring can provide big area of water quality information,the characteristic of RS is timing and prompt and permanence. The information which provided by RS is not assimilate with general monitoring water quality.
     RS监测可以大面积地提供水质信息,并且具有适时、迅速、持久等特点,它所提供的信息量是常规水质监测所不能比拟的。
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     The calculations in theory point out that the siO2in the slag can' t change Ti(C,N) into TiO2,however,it can assimilate with Ti(C.N). The large inclusions affect the quality of the steel plate and tube greatly.
     经理论计算证实:保护渣中的SiO_2不能将TiN转化成TiO_2。
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     Japanese religions could not assimilate with Chinese culture since they were with distinctive invasion character, they hurt Chinese people's religious feeling deeply by forcing people to change their own traditional religious beliefs.
     当时,随着日本军事侵略而传来的日本宗教有神道教、佛教、基督教、天主教等类派别,由于带有明确的侵略目的,强迫中国民众改变传统观念信仰,使中国人民的宗教感情受到极大的伤害,因而,无法真正融合于中国文化。
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     The factors led to that overseas Chinese of Indonasia can not assimilate with nations in value social,political economical and cultural aspects.
     导致印度尼西亚的华人不能与原住民真正融合、同化的因素涉及到社会、政治、经济、文化等多方面。
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     The modernization of Chinese philosophy should return to the road of "science and democracy" rather than the traditional Confucianism, and assimilate with an open mind all the useful resources of thoughts both in Chinese and foreign history, especially the scientific spirit of modern western philosophy.
     中国哲学的现代化问题应该回到"科学与民主"的旗帜下,而不是传统儒学,以"拿来主义"精神,吸取中外历史上一切有用的思想资源,尤其是现代西方哲学中的科学精神。
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  相似匹配句对
     ASSIMILATE TRANSPORTATION IN THE PHLOEM AS RELATED TO THE XYLEM
     韧皮部同化物运输与木质部的关系研究
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     On Several Ways to Assimilate Bibliographical Information
     论文献信息吸收的若干形式
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     Effect of DPC on Translocation Redistribution or 14 C Assimilate of Cotton Interplanted with Wheat
     DPC对麦套棉~(14)C同化物运转分配及再分配的影响
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     The results showed that wheat assimilate accumulation increased along with amount of applied manure.
     结果表明 ,开花后同一天 ,冬小麦同化物的积累量随有机肥水平提高而增加 ;
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  assimilate with
Hence, they find it socially difficult to assimilate with the local population.
      


The initial ~(87)Sr/~(86)Sr ratio of 0.70428 and δ~(18)O of 7.7—9.2 for the Zijinshan igneous complex suggest that materials of the complex primarily originated from upper mantle and were assimilated with those of crustal sources in small amount. According to the REE abundance characteristics of eight types of rock in the complex—monzonite, aegirineaugite syenite, melteigite, malignite, nephelinesyenite, pseudoleucite phonolite, trachyte-porphyry and medium-grained aegirinesyenite——they can be classified...

The initial ~(87)Sr/~(86)Sr ratio of 0.70428 and δ~(18)O of 7.7—9.2 for the Zijinshan igneous complex suggest that materials of the complex primarily originated from upper mantle and were assimilated with those of crustal sources in small amount. According to the REE abundance characteristics of eight types of rock in the complex—monzonite, aegirineaugite syenite, melteigite, malignite, nephelinesyenite, pseudoleucite phonolite, trachyte-porphyry and medium-grained aegirinesyenite——they can be classified into three groups. On the whole, all of three groups of rocks are rich in light REE and have an unremarkable Eu anomaly, and the ratio of Eu/Eu* for these rocks ranges from 0.95 to 1.12. The total REE content, especially the heavy REE content in rocks decreases from the first group to the third one, i.e.from the early one to the late one (∑HREE: 41.6→18.3→13.8 ppm). In the meantime the slope for the chondrite normalized REE pattern also increases, but the situation among each group turns out contrary. The quantitative mode calculation for the degree of partial melting of upper mantle indicates that the degree decreasses from the first group of rocks to the third one (1.60→1.58→1.575%). However, among each group of rock the degree of partial melting increases from the ealiest rock to the last one. It is very interesting to note that there exist two kinds of evolution trends in the igneous complex.

紫金山杂岩体的氧同位素δ~(18)O为7.7—9.2‰,锶同位素初始比值~(87)Sr/~(86)Sr为0.70428,这表明该杂岩体的物质来源主要是上地幔。根据稀土元素特征,可将该杂岩体的八种岩石分为三组。总的来看三组岩石均呈富轻稀土型,Eu异常不明显,Eu/Eu变化范围为0.95—1.12。从第一组岩石到第三组岩石,即从早到晚稀土总量降低,尤其是重稀土更突出(∑HREE从41.6→18.3→13.8),球粒陨石标准化曲线的倾斜度变陡,但在每一组中的变化趋势正好与前者相反。在同一个杂岩体中出现两种变化趋势,这是很有意义的。

This paper introduce the 2D Vision System. The informative image of the place of robot and object are assimilated with pickup camera,Thus the information of their relative place in the space are determined,The programme control of robot may be realized.

本文介绍二维视觉系统。通过摄像机摄取机器人和物体位置信息的图像,从而确定它们在空间相对位置信息,实现机器人的规划控制。

Seismic tomography technique,which is mainly used to determine the three-dimensional ve- locity structure,has been rapidly developed in recent years,but the geological meaning of the seis- mic velocity anomalies,i.e.the relationship between the velocity anomalies and geological structu- res,has been not still studies in detail upto now.In this paper the fundamentals of geological in- terpretation of seismic velocity structure are discussed for the first time.Based on their velocity characteristics and seismic...

Seismic tomography technique,which is mainly used to determine the three-dimensional ve- locity structure,has been rapidly developed in recent years,but the geological meaning of the seis- mic velocity anomalies,i.e.the relationship between the velocity anomalies and geological structu- res,has been not still studies in detail upto now.In this paper the fundamentals of geological in- terpretation of seismic velocity structure are discussed for the first time.Based on their velocity characteristics and seismic velocity distribution,the crust,lower lithosphere,asthenosphere and asthenospheric upwell is identified.The resolution to distinguish different structures is related to seismic ray path,wave length,time service precision and element size divided.In a better con- dition,the resolution is in the ranges of 15—25km.How long tectonic history which may be traced by seismic tomography depends on the thermo-dynamic process in which the remainder of an ancient orogeny would be assimilated with the environment.A large orogen.aged 300— 400 m.y.can be recognized through its remainder structural signatures in the crust,lower lithosphere and asthenosphere.By seismic tomography and its geological interpretation it is di- scovered that the lower lithosphere of Yangze block in the Ailaoshan area has westwards subdu- cted taro the depths of 250—300 km beneath the Simao-Lincang block and an asthenospheric upwell stands in front of the subducting lithosphere.This implies that Ailaoshan belt is a litho- spheric subduction collision orogen subducting westwards instead of subducting eastwards in- fered formerly by surface faults.The results are proved by seismic reflection and electromagne- tic sounding in the same areas.

本文首先简要地介绍了地震层析方法的原理,着重探讨了三维速度异常地质解释的几个基本问题,包括划分构造层的物理基础、确定分辨尺度的依据以及估计地质时限依据的岩石热力学过程。然后介绍了应用地震层析及地质解释方法研究滇西造山带的地壳、下岩石圈及软流圈构造所得到的主要结果,并与人工地震测深及大地电磁测深结果进行了比较。这一工作说明地震层析可以作为岩石圈与软流圈构造研究的一种有效手段,在造山带深部构造的研究中将发挥独特的作用。

 
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