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tripartite
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  三分的
     Grasping the Objects and Achievements of the Study of Dialectics of Nature from the Angle of a Tripartite Principle
     从一总三分的视角掌握《自然辩证法》
短句来源
     This paper will comprehensively comment on and systematically grasp the objects and achievements of the study of the book, from the angle of a tripartite general principle——materialist dealectics and dialectics of nature, historical dialectics, dialectics of thinking.
     本文以一总三分的视角为出发点 ,即唯物辩证法和自然辩证法、历史辩证法、思维辩证法 ,综合评价并系统掌握该书的研究对象与研究成果。
短句来源
  “tripartite”译为未确定词的双语例句
     The complete tripartite graph K_(2,2,r),r=4,5,6,7, are not U3LC graph
     完全三部图K_(2,2,r),r=4,5,6,7,不是U3LC图
短句来源
     Let K(m,n,r) denote a complete tripartite graph,this paper proved that (1)If m≤n≤r,0≤r-m≤4 and m≥2,the graphs K(m,n,r) is chromatically unique except for k(2,2,6),K(2,3,6),K(3,3,7),K(3,4,7).
     令K(m,n,r)表示完全三部图,证明了(1)设m≤n≤r,0≤r-m≤4,若m≥2,则除去K(2,2,6)、K(2,3,6)、K(3,3,7)、K(3,4,7)外,K(m,n,r)是色唯一图。
短句来源
     Let(K(m,n,r)) denote the complete tripartite graph,G=K(m,n,r)-A(|A|=2),3≤m≤n≤r.
     令K(m,n,r)表示完全三部图,G=K(m,n,r)-A(|A|=2),3 m n r.
短句来源
     The Complete Tripartite Graphs K_(2,2,r)(r=4,5,6) Have Property M(3)
     完全三部图K_(2,2,r)(r=4,5,6)具有M(3)性质
短句来源
     On the Chromatic Uniqueness of Tripartite Graphs K(m,n,r)-A(|A|=2)
     三部图K(m,n,r)-A(|A|=2)的色唯一性
短句来源
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  相似匹配句对
     On the Tripartite Fraud
     论三角诈骗
短句来源
     On the Chromaticity of the Complete Tripartite Graph K(n-k,n,n)
     完全三部图K(n- k,n,n)的色性(英文)
短句来源
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  tripartite
The feasibility of using double inoculation as a means of increasing the plant productivity is demonstrated, in which the potential of a tripartite symbiotic system (pea plants-root nodule bacteria-arbuscular mycorrhiza) is mobilized.
      
Anm-crown is the complete tripartite graphK1, 1,m with parts of order 1, 1,m, and anm-claw is the complete bipartite graphK1,m with parts of order 1,m, wherem ≥ 3.
      
Continuous variable tripartite entanglement and Einstein-Podolsky-Rosen correlations from triple nonlinearities
      
We develop three-mode generalizations of the Einstein-Podolsky-Rosen paradox, allowing us to define inequalities which may be used to indicate continuous-variable tripartite entanglement.
      
The experiment results showed the "tripartite effect" of rare earth.
      
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The phase velocities of Rayleigh waves in China were obtained by using the seis- mograms from twelve stations in China.Two earthquakes from New Britain Islands were chosen.The amplitudes of Rayleigh Waves with the period of about 35 seconds are considerably smaller than their following phases with shorter periods.This particular feature of the seismograms can be traced from most of the stations.It makes the cor- relation more feasible.Detailed correlations are obtained by analyzing the variation of periods with...

The phase velocities of Rayleigh waves in China were obtained by using the seis- mograms from twelve stations in China.Two earthquakes from New Britain Islands were chosen.The amplitudes of Rayleigh Waves with the period of about 35 seconds are considerably smaller than their following phases with shorter periods.This particular feature of the seismograms can be traced from most of the stations.It makes the cor- relation more feasible.Detailed correlations are obtained by analyzing the variation of periods with distances and also the arrival times of each crest of Rayleigh waves in the seismograms.The phase velocities of separate regions as computed from two different earthquakes are in good agreement.The results show that in calculating the phase velo- cities with tripartite method,the corrections due to different oceanic paths can not be neglected if the angular distances between them were great.Because the parameters of the earth crust in China are not well-known,we have to compare these calculated phase velocities of Rayleigh waves in China with the revised phase velocity nomograms of Rayleigh waves by Press,based on the materials obtained in Africa.The crust thick- nesses in separate regions are thus computed,the results being merely tentative.How- ever,unless more geophysical data were available,these data as given by this method still show a rather close correlation with the principal tectonic features in China.In the region of Tibetan Plateau,the phase velocities are very low,and the calculated thick- ness of the earth crust there is 74 kms;whereas in the region of southeastern coast,the phase velocities are high,and the calculated thickness is only 20 kms.

本文利用新不列颠岛两个地震在十二个基本台站所记录到的瑞利波,计算了我国不同地区的相速度.着重讨论鉴别和对比不同台站记录中同一震相的方法.在大部分台站的记录中,见到有周期约为35秒的相位,和后面的位相比较,它的周期较大,振幅较小.波形的对比对初步鉴别震相有很大的帮助.详细的震相对比是根据周期随距离变化的规律和各震相到时的规律.两个地震所得的相速度很符合.计算的结果表明:利用三台计算相速度时,如果射线的路程差别较大,海洋路程的校正是不能忽略的.因为有关我国地壳构造的资料还很少,我们所得的瑞利波相速度只能与普瑞司修正后非洲大陆的相速度理论相比较,由此得到我国不同地区的地壳厚度.这样所得的厚度,虽然不能视为最后的结果,但是它们仍然表现与主要地质单元之间有密切的联系.

The Shihchienfeng Group,a red-bed series covering vast area of North China,isgenerally considered to be Permo-Triassic in age.However,such a view needs to bereexamined in the light of the discovery of two marine interbeds found in the nor-thern Weihe River Basin.The first one belongs to the upper member of the lowerformation(Sunjiagou Formation)of the tripartite Shihchienfeng Group.This marinebed,yeilding bivalves,lingulids and other brachiopods,estherids and plant remains,has been spotted at 8 localities,the...

The Shihchienfeng Group,a red-bed series covering vast area of North China,isgenerally considered to be Permo-Triassic in age.However,such a view needs to bereexamined in the light of the discovery of two marine interbeds found in the nor-thern Weihe River Basin.The first one belongs to the upper member of the lowerformation(Sunjiagou Formation)of the tripartite Shihchienfeng Group.This marinebed,yeilding bivalves,lingulids and other brachiopods,estherids and plant remains,has been spotted at 8 localities,the most important of which is in Houzhougonmiao,Qishan County.Early study on a small collection of this fauna gives the followinglist;Aviculopecten cf.mccoyi(Meek et Hayden),Liebea?sp.,Wilkingia?sp.AsAviculopecten cf.mccoyi is a permian scallop and the other two are of Palaeozoicgenera,they were regarded as an imp(?)rtant evidence to dismember the ShihchienfengGroup and to place its lowest subdivision,the Sunjiagou Formation,in late UpperPermian.Review of the collection as well as study of more and better specimens obtainedsince then at the samc place show,however,that the so-called Aviculopecten cf.mccoyi is nothing but Eumorphotis multiformis,a lower Scythian index fossil of SouthChina,and the other species indicate an Early Triassic rather than Late Permian age.A revised list is given below:Bivalves:Eumorphotis multiformis Bittner,Leptochoncria aff.virgalensis(Wit-tenburg),Promyalina putiatinensis(Kiparisova),P.intermedia Chen,Homomya im-pressa(Alberti).Obviously the bed containing all the obove species.should lie at the middle-upperpart of Lower Scythian,thus demonstrating the Sunjiagou Formation to T_1.and itslogical reunification with the Lower Triassic Shihchienfeng Group,so its base makesthe Palaeozoic-Mesozoic boundary.The second marine interbed found in Zhishiya,Linyou County,within reddishsandstones lies discomformably on the Sunjiagou Formation.It is equivalent to theLiujiagou Formation rather than to any other unit on stratigraphical and petrogra-phical grounds,as is discussed in this paper.Fossils collected from it are as follows: Bivalves:Pteria cf.murchisoni(Geinitz),Bakevellia costata(Schlotheim),Gervil-lia exporrecta(Lepsius),Palaeoneilo elliptica(Goldfuss),Mylilus cduliformis subprae-cusor Yin(subsp.nov.),Unionites spp.Brachiopods:Mentzelia sp.Ophiuroids:Ophiolepis shaanxiensis Yang(sp.nov.)The second marine bed is of Late Scythian age,as judged from the occurrence ofPteria cf.murchisoni and the fauna as a whole when correlated with those from SWChina and Southern Qilianshan Mrs.Of particular interest is the discovery of fivedelicate ophiuroids which have rarely been found in the Triassic except in theGerman Sea Basin.

本文记述了岐山后周公庙孙家沟组及麟游紫石崖刘家沟组的海相化石,计有瓣鳃类9属10种,蛇尾纲1种,腕足类一未定种。根据这些海相化石的研究,认为渭北地区整个石千峰群均应属早三叠世。

In this paper, we constructively show that, for a complete tripartite grape G(X, Y, Z; E), if the number of edges is divisible by positive integer t and one of three number |X|, |Y| and |Z| .is also divisible by t,then the complete trip- artite graph may be factored into t isomorphic fectors. Therefore, a partial con- clusion of Harary's "Tripartite conjecture" was confirmed.

本文构造性地证明,对于完全3部图 G(X,Y,Z;E),如果边数能被正整数t整除,且|X|, |Y|和|Z|三个数之一也能被t整除,则完全3部图可分解为t个同构因子,从而证实了Harary “3部图猜想”的部分结论。

 
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