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整合的
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  integration
     Genetic Mapping and Position Effect of Rice T-DNA Integration Genetic Analysis and Gene Mapping of a Rice Multi-pistil Mutant
     水稻T-DNA整合的遗传定位与位置效应一个水稻多子房突变体的遗传分析与基因定位
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     The Expression of vgbM Gene in Plants and the Preliminary Analysis of the Cry1A Gene Integration in GK12 Cotton
     vgbM基因在植物中的表达及抗虫棉GK12中外源基因整合的初步分析
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     Research on Integration Information Management System for Digital Hospital of HRPS
     HRPS数字化医院信息管理系统整合的研究
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     Preliminary Study on Chromosomal Integration of Epstein-Barr Virus in a Burkitt's Lymphoma Cell Line (Raji)
     Epstein-Barr病毒在Burkitt淋巴瘤细胞(Raji)染色体上整合的初步研究
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     On the Influence Factors and the Tactics of Enterprise Culture Integration in Mergers & Acquisitions
     并购企业文化整合的影响因素及策略研究
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  conformable
     Collection of relative aboundant fossils and researches of geoche-mical characteristics near the boundary at Yanshi section have raised the accuracy in locating the boundary between two systems, revealed the characters of Permian-Triassic organism alteration and testified the conformable contact between two systems.
     界线附近较丰富的动物群的采集及地球化学特征的测试,提高了界级划分精度,揭示生物更替规律,证明两系之间为整合的接触关系。
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     By comparing the theories of EQ,AQand IQ,this paper points out the mistake of nonperfect andunreasonableness of EQand AQ in conceptional and theoretical formation,criticizes the trend of exaggerating the roleof EQ and AQ leading to their negative role in real life,and meanwhile,admits that EQ and AQ have positive sense inexpanding the field of psychological research,initiating modern and conformable health education,and popularizingpsychological knowledge.
     本文通过对情感智商、逆境商数和智商理论的比较,指出情感智商与逆境商数在其概念和理论建构上的不完善和不合理的误区,批评把EO、AQ的作用夸大从而导致现实中的负作用的倾向,同时也肯定了EQ、AQ理论在对心理学研究领域和研究视野的扩展,以及对倡导现代的整合的健康教育和普及心理学知识所起的积极意义。
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     The network-assisted instruction is a conformable Teaching pattern based on combining information technics and certain disciplinary course. Using theoretical analysis and teaching experiment,the paper investigated preliminary the teaching problems concerned with network-assisted instruction for general physics.
     网络辅助教学是基于信息技术(网络技术)与学科课程整合的一种教学方式,文章通过理论分析和教育实验对普通物理课程网络辅助教学的有关教学问题进行了初步的研究。
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     The System of Prime Farmland Protection Planning Based on Integrating GIS with Decision-making Models
     基于GIS与决策模型整合的基本农田保护规划系统
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     Dependence of the recA Gene for the Replication of the Bacterial Chromosome Initiated by the Integrated F' Plasmid in Escherichia colt
     大肠杆菌中整合的F′质粒带动细菌染色体复制需要recA基因
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     Sociological Interpretation of Disintegration and Reorganization of Structure of Sport Society of China in Current Stage
     中国现阶段体育社会结构分化和整合的社会学阐释
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     The inhibitor of PARP enzyme does delete the integrated LacZ pene
     PARP酶抑制剂未引起整合的外源LacZ基因的丢失
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     From the character of information technology and science course teaching and through practice and thinking, the paper discusses conformity nature and solving strategy, reforming teaching means and method, optimizing class teaching, improving teaching effect.
     从信息技术和科学教学的特点出发,通过对信息技术与初中科学教学整合的实践和反思,探究整合实质和问题解决策略,改革教学手段和方法,优化课堂教学,提高教学效果。
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  integration
Of special interest are the Mellin operators of differentiation and integration, more correctly of anti-differentiation, enabling one to establish the fundamental theorem of the differential and integral calculus in the Mellin frame.
      
Wavelets, generalized white noise and fractional integration: The synthesis of fractional Brownian motion
      
The desired $\mathfrak{M}_{q}\left(\mathbb{T}\right)$-functional calculus for $T$ then results from an extension criterion for spectral integration obtained in the general Banach space setting.
      
Tools used to obtain such results are the Van der Corput lemma, integration by parts, Young's inequality and the interpolation theory.
      
N-aminoimidazoles and pyridine oxide derivatives) which seem to interfere with a post-integration, transcription transactivation event.
      
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  conformable
Conformable lodes of spinel-forsterite skarn and calciphyre impregnated with magnesian magnetite replaced dolomite near the central magma conduit and apical portions of igneous bodies.
      
This size scale makes them conformable to common biomolecules.
      
Test was performed to evaluate the structural integrity of a conformable auxiliary fuel tank mounted beneath the floor and to determine its effect on the impact response of the airframe structure.
      
The objective of the test was to determine the interaction between a typical transport aircraft fuselage, particularly its floor structure, and a conformable auxiliary fuel tank under severe, but survivable, impact conditions.
      
Most of them are delineated by conformable or submarine erosion surfaces, and well controlled by conodont and fusulinid zones.
      
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The stereospecific polymerization of butadiene catalysed by homogeneous systems formed by combination of trialkyl aluminium with β-diketone chelates of rare earth elements has been studied. It has been shown that combinations of the following rare earth chelates with triethyl aluminium could induce cis-1,4 stereospecific polymerization of butadiene: NdB3 (B=benzoylacetonate), NdB, NdBTA(BTA=benzoyltrifluoroacetonate), NdTTA(TTA = thenoyltrifluoroacetonate), PrB3, PrB, PrBTA, PrTTA, YB3, YBTA, and LaBTA. These...

The stereospecific polymerization of butadiene catalysed by homogeneous systems formed by combination of trialkyl aluminium with β-diketone chelates of rare earth elements has been studied. It has been shown that combinations of the following rare earth chelates with triethyl aluminium could induce cis-1,4 stereospecific polymerization of butadiene: NdB3 (B=benzoylacetonate), NdB, NdBTA(BTA=benzoyltrifluoroacetonate), NdTTA(TTA = thenoyltrifluoroacetonate), PrB3, PrB, PrBTA, PrTTA, YB3, YBTA, and LaBTA. These homogeneous systems appear to possess much higher catalytic activity than those of the heterogeneous systems formed by combination of triethyl aluminium with halides of lanthanons studied earlier. Up to a certain extent of catalyst concentration, the catalytic activities of these systems increase with increasing ratio of Al/chelate or chelate/ butadiene (molar ratio). The polymerization has an induction period and it is found that the rate of polymerization is of first order with respect to the monomer concentration and approximately of first order to the chelate concentration. With the NdB3-Al(C2H5)3 system, the activation energy of polymerization has been determined to be 13.0±0.5 kcal/mole. Both polymerization rate and microstructure of polybutadiene depend upon the nature of the rare earth metal in the chelates rather than that of the ligands in various chelates, and the praseodymium and neodymium chelate systems gave higher catalytic activity. It is interesting to note that polybutadienes obtained with these homogeneous systems always have a 1,2-structure content less than 1%, with little or even no gel formation. The intrinsic viscosities of the polymers obtained varying from 4-5 to 1, depend on the Al/chelate and chelate/butadiene ratios. Variation in alkyl groups on the aluminium component results in a marked difference in catalytic activity. The Al(i-C4H9)3 system exhibits low activity and Al(C2H5)2Cl system is inactive.

本工作研究了β-二酮类希土螯合物与三烷基铝组成的均相体系对丁二烯定向聚合的催化活性及一些聚合规律。实验结果表明下列希土螯合物与三乙基铝组合时都具有使丁二烯进行顺式-1,4定向聚合的催化活性:NdB_3;NdB;NdBTA;NdTTA;PrB_3;PrB;PrBTA;PrTTA;YB_3;YBTA 以及 LaBTA 等。这些均相催化体系的活性远比非均相希土氯化物体系的高。在一定的催化剂浓度范围内,催化活性随着Al/希土及希土/丁(克分子比)的增高而增大。聚合反应速率对单体浓度呈一级关系,对希土螯合物浓度也近似呈 一级关系,并呈现一诱导期。丁二烯在 NdB_3-Al(C_2H_5)_3体系中聚合的总活化能为 13±0.5千卡/克分子。研究不同希土元素的这些螯合物表明同一元素的不同螯合物体系的聚合反应速率和聚合物链结构都没有显著的差别。但不同希土元素的同一整合物体系的聚合活性相差较大,含有镨和钕螯合物体系的活性比其他体系大。由这些均相催化体系所得聚丁二烯的1,2链节含量不超过1%,都不含或含很少量凝胶,聚合物的[η]随着Al/希土(克分子比)以及希土/丁(克分子比)的增大而降低,[η]可以从 4—5降至 1以下。A...

本工作研究了β-二酮类希土螯合物与三烷基铝组成的均相体系对丁二烯定向聚合的催化活性及一些聚合规律。实验结果表明下列希土螯合物与三乙基铝组合时都具有使丁二烯进行顺式-1,4定向聚合的催化活性:NdB_3;NdB;NdBTA;NdTTA;PrB_3;PrB;PrBTA;PrTTA;YB_3;YBTA 以及 LaBTA 等。这些均相催化体系的活性远比非均相希土氯化物体系的高。在一定的催化剂浓度范围内,催化活性随着Al/希土及希土/丁(克分子比)的增高而增大。聚合反应速率对单体浓度呈一级关系,对希土螯合物浓度也近似呈 一级关系,并呈现一诱导期。丁二烯在 NdB_3-Al(C_2H_5)_3体系中聚合的总活化能为 13±0.5千卡/克分子。研究不同希土元素的这些螯合物表明同一元素的不同螯合物体系的聚合反应速率和聚合物链结构都没有显著的差别。但不同希土元素的同一整合物体系的聚合活性相差较大,含有镨和钕螯合物体系的活性比其他体系大。由这些均相催化体系所得聚丁二烯的1,2链节含量不超过1%,都不含或含很少量凝胶,聚合物的[η]随着Al/希土(克分子比)以及希土/丁(克分子比)的增大而降低,[η]可以从 4—5降至 1以下。Al(i-C_4H_9)_3也能与这些螯合物组成活性催化体系,但活性很低。Al(C_2H_5)_2Cl则不能与这些螯合物构成活性催化体系。

According to the characteristics of paleobotany, the flora features of Taxigou Series undoubtedly belong to the late age of the Dictyophyllum-Clathropteris groups while the flora of the Yaojie Group are members of the Coniopteris-Phoenicopsis groups; so that the age of Taxigou Series is earlier than that of the Yaojie Group.According to the correlation of the stratigraphy, the writer deems that the Taxigou Series and the Yanganshi Formation of this locality and the Nanying-er Group of Wu-wei district in this...

According to the characteristics of paleobotany, the flora features of Taxigou Series undoubtedly belong to the late age of the Dictyophyllum-Clathropteris groups while the flora of the Yaojie Group are members of the Coniopteris-Phoenicopsis groups; so that the age of Taxigou Series is earlier than that of the Yaojie Group.According to the correlation of the stratigraphy, the writer deems that the Taxigou Series and the Yanganshi Formation of this locality and the Nanying-er Group of Wu-wei district in this province are contemporary deposites. Therefore, the upper part of the Na-nying-er Group has the possibility of belonging to the early Jurassic perieod and the lower part of the Taxigou Series might be of late Triassic.The age of Yaojie Group belongs to the middle Jurassic and its contacted relation with Nanying-er Group is discomformable. The Xiang-ta'ng Group of the upper Jurassic is also discomformable overlying the Yaojie Group.Beeause of the flora feutures of the Honggou Group well resemble that of the Yaojie Groups and the contacted relation between them is comformable, so that the Honggou Group is really the upper part of the Yaojie Group and is unneccessary to be divided from the lat-ter as a single stratigraphic unit.

根据古植物特征,“大西沟系”的古植物群属Djctyophyllum-Clathropteris植物群的晚期群落,而窑街群的古植物群则属于Coniopteris-Phoenicopsis植物群,因而“大西沟系”的时代早于窑街群.根据地层对比“大西沟系”与“羊肝石层”及武威南营几群为同期沉积,因而南营几群的上部有属于早侏罗世的可能,而“大西沟系”的下部有属于晚三迭世沉积的可能. 窑街群属中侏罗统,与南营几群呈假整合接触.晚侏罗统享堂群则假整合于窑街群之上. 红沟群由于古植物面貌与窑街群一致,又二者呈整合接触,因而红沟群不宜单独划出,而归于窑街群顶部.

The original conception of the Sinian stratigraphy and correlation of southern China should be revised on account of the following geological informations: (1) The unconformable relation below the Nantou Sandstone, which commonly occurs within the axial parts of the Kiangnan geanticline, and which was taken to represent the lower boundary of the traditional Sinian system, changes into conformable contact on the southern limb of the Kiangnan geanticline; (2) The absolute ages of the granites unconformably overlain...

The original conception of the Sinian stratigraphy and correlation of southern China should be revised on account of the following geological informations: (1) The unconformable relation below the Nantou Sandstone, which commonly occurs within the axial parts of the Kiangnan geanticline, and which was taken to represent the lower boundary of the traditional Sinian system, changes into conformable contact on the southern limb of the Kiangnan geanticline; (2) The absolute ages of the granites unconformably overlain by the Nantou Sandstone have been determined to be around 700—800 million years, which are just about corresponding to the age of the middle-upper part of the key Sinian section of the Jihshien area in North China. The present writers give new considerations about the Sinian stratigraphy and correlation of southern China according to the following principles and reasons: (1) In the areas, where Caledonian geosyncline inherited from the Hsuehfeng geosyncline, the Nantou Sandstone formation is generally conformable with the underlying low-graded metamorphosed sediments, and in such areas, the overlying sediments are closely related in characters with the underlying strata, and here the total thickness of these formations now considered to be Sinian in age, is usually much greater. On the other hand, in those areas, where the younger sedimentary basin was superimposed upon the folded Hsuehfeng geosynclinal sediments, as occurring within the axial parts of the Kiangnan geanticline, the Nantou Sandstone then lies unconformably upon the more intensely metamorphosed sediments, and there the Sinian system is generally incomplete in section. (2) Although the tradi tional Sinian system of the South China geosynclinal regeion possesses the characters of geosynclinal sediments, it attains a total thickness of only 1000—3000 meters, which appears to be rather insufficient when compared with the vast thickness of some 10,000 meters of the Sinian system in the Yenshan subsidence zone of northern China. (3) The absolute age of the Jiulinshan granodiorite is dertermined to be 837 millions years, which is just corresponding to the age of the middle-upper part of the Sinian system in North China, while the age of the lower limit of the Sinian of northern China is generally accepted to be 1200—1400 millions years. From the above-stated reasons, the present writers are inclined to take the unconformity surface below the upper Banchi Group, (which represents the Tung-an movement), as the lower boundary of the Sinian system of southern China. Thus, the upper Banchi Group is now considered to be the lower part of the Sinian, and the traditional Sinian system of southern China is now taken to represent the upper Sinian. The Hsuehfeng movement of the Kiangnan geanticline marks the boundary between the lower and the upper Sinian. Based upon the above-mentioned scheme of the Sinian subdivisions, some historical developments of the region can be brought out: (1) The formational sequences of the lower Sinian of the South China Caledonian geosynclinal region are chiefly eugeosynclinal and partly miogeosynclinal in nature, but the formational sequences on the southern limb of the Kiangnan geanticline are slightly different in nature from that of the northern limb. Judging from the characters of sediments, the sedimentary environment on the southern limb was rather active while that on the northern limb was relatively stable. During the earlier period of the Sinian time in the Hsuehfeng-Caledonian geosynclinal region, a marginal belt on the north of the embryo Kiangnan geanticline and an inner (mobile) belt on the south can already be distinguished. (2) As a consequence of the Tung-an movement, the embyro form of the Kiangnan geanticline was formed. (3) In western Hunan, the Tungan movement was intense and it diminished in intensity eastward, and in southern Anhui it was represented by epeirogenic movement. However, the subsequent development displays the phenomenon to the contrary. The lower Sinian in southern Anhui and western Chekiang is represented by the typical eugeosynclinal formations, while in northwestern Kiangsi and western Hunan it is represented by either miogeosynclinal or eugeosynclinal formations. Such differences in intensities in earth movements along the regional structural line in a geosynclinal system show the unbalanced development of the Caledonian geosynclinal region in South China.

本文通过接触关系、厚度分析,结合绝对年龄资料,考虑地层剖面发育与构造关系,运用继承与上迭原则,认为继承构造部位剖面最完整这一理由,对江南地背斜带震旦纪地层提出了新的划分方案。新方案中的下震旦统包括上板溪羣及与其相当的上双桥山羣、瀝口羣、松木坞羣等浅变质岩系,以东安运动形成的不整合面作为震旦系与前震旦系的分界;旧称震旦系则归入上震旦统。上、下震旦统之间为雪峰运动形成的不整合面分开。在对上述地层的建造一构造分析的基础上,初步提出华南加里东地槽区江南地背斜带已经出现了南侧比较活动,北侧相对稳定的不对称性。另一方面构造发展在沿走向上也表现了不均一性,东安运动在江南地背斜带的西段表现明显,而到了东段就逐渐消失。

 
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