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  条件
     Formation and Evolution of JiaoLai Basin and Formation Condition of Combination Gas
     胶莱盆地形成演化与油气形成条件
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     Study on Postharvest Physiology and Preserving-freshness of Fresh Vegetable under the Condition of Simulated Cold Stroage of Warship
     模拟舰船条件下蔬菜采后生理和保鲜的研究
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     A Study on Portfolio Selection Model on Condition of Non-normal Distributions
     非正态分布条件下的投资组合模型研究
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     The Survey of Metallogenic Geologic Condition of Lead-zinc Deposit and Metallogenic Prediction with Synthesis Information in the West of Guizhou
     贵州西部地区铅锌矿成矿地质条件及综合信息成矿预测研究
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     The Study of Theory, Method and Application about Surface Water Resources Assessment under the Condition of Environment Changes
     环境变化条件下的地表水资源评价理论方法及应用研究
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  情况
     THE INVESTIGATION OF ALLOWABLE CONCENTRATION OF THE DUST OF FERROALLOY FROM THE CONDITION OF INCIDENCE IN PNEUMOCONIOSIS OF FERROALLOY
     从铁合金尘肺发病情况探讨铁合金粉尘容许浓度
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     Investigation of Infective Condition of Intestinal Parasites in Nanchang
     南昌市肠寄生虫感染情况调查
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     The Sample Construction of Q process in Condition of Q Conservation and m Running out
     Q保守m流出情况下,Q过程的样本构造
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     The Relationship between Carnot Heat Pump Optimum Heat Supply Factor and Heat Supply Flow Rate under the Heat Transfer Condition of q(T, Tw)=α(1/Tw-1/T)
     q(T,T_w)=α(1/T_w-1/T)传热情况下卡诺热泵的最佳供热系数与供热率间的关系
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     A Survey of Fundamental Condition of Secondary Stomatological Education and A Forecast of the Requirement for Higher,Secondary and Elementary Stomatological Education of China
     我国中等口腔医学教育基本情况调查及高、中、初等口腔医学教育需求预测
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  状况
     The Finite Element Analysis for Condition of Air Flow in the Winning Area
     采场空气流动状况有限元分析
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     An Investigation into the Nutrition Condition of the University Students
     对大学生营养状况的调查
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     STUDY ON THE WATER CONDITION OF ANEUROLEPIDIUM CHINENSE COMMUNITY
     羊草群落水分状况的初步研究
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     MACROSCOPIC CONTROL AND PREDICTION FOR THE PAVEMENT CONDITION OF ASPHALT HIGHWAY NETWORKS
     沥青公路网路面状况的宏观控制和预测——控制理论用于公路管理(Ⅰ)
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     Macroscopic Control and Prediction of the Pavement Condition of Asphalt Highway Networks——Applications of Cybernetics to Highway Management (Ⅰ)
     沥青公路网路面状况的宏观控制和预测——控制理论用于公路管理(Ⅰ)
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  条件下
     Study on Postharvest Physiology and Preserving-freshness of Fresh Vegetable under the Condition of Simulated Cold Stroage of Warship
     模拟舰船条件下蔬菜采后生理和保鲜的研究
短句来源
     A Study on Portfolio Selection Model on Condition of Non-normal Distributions
     非正态分布条件下的投资组合模型研究
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     The Study of Theory, Method and Application about Surface Water Resources Assessment under the Condition of Environment Changes
     环境变化条件下的地表水资源评价理论方法及应用研究
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     Research on the Dynamic Schedule Optimization of Construction Project on the Condition of Minimum Cost/Maximum Benefit.
     费用最低/收益最大条件下的工程项目动态进度优化研究
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     A Study on the Response of Plants to Ozone Injury Under the Condition of Fumigation Experiment
     熏气实验条件下植物对臭氧反应的初步研究
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Also, we show by an example that the sufficient condition of Lagarias and Szabó [13] for the existence of universal spectra is not necessary.
      
A condition of the existence of stable positive steady-state solutions for a one predator two prey system
      
This paper provides a natural condition of the existence of stable positive steady-state solutions for the one predator two prey system.
      
The equivalent condition of this optimal design is given.
      
Different from rational quadratic Bézier curves, the value is generally related with the location of the ray, and the necessary and sufficient condition of the ratio being independent of the ray's location is showed.
      
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By replacing the fifth postulate in the preceding paper with the condition of spherical symmetry of space we again obtain the Friedmann universe in relativistic cosmology.

将前文中第五个假定改为“空间具球面的对称性”后我们仍遵出费烈特猛宇宙。

Using the micromethod of Farmer and Abt, plasma vitamin C content of 9S boys and girls in a middle school was determined throughout the year 1954 to 1955. A dietary survey was also carried out every month of the year, for calculating the vitamin intake. The results of the present study are as follow:1. When the diet contains ample amount of fresh leafy vegetables in season, a satisfactory plasma vitamin C level can be maintained. When the diet is limited in fresh vegetables, plasma vitamin C readily decreases...

Using the micromethod of Farmer and Abt, plasma vitamin C content of 9S boys and girls in a middle school was determined throughout the year 1954 to 1955. A dietary survey was also carried out every month of the year, for calculating the vitamin intake. The results of the present study are as follow:1. When the diet contains ample amount of fresh leafy vegetables in season, a satisfactory plasma vitamin C level can be maintained. When the diet is limited in fresh vegetables, plasma vitamin C readily decreases in those seasons.2. There is a significant seasonal variation of plasma vitamin C content Highest values are obtained in winter, the maximal content occurring in December. The minimal value is observed in June. This corresponds to the variation in the. level of vitamin C intake in different seasons. There is no significant difference between Autumn and Winter.3. No definite correlation between plasma vitamin C content and the condition of the gums was observed in the present study.4. The plasma vitamin C content of Chinese and English school children observed by some other authors was lower than that obtained in the present investigation. It is believed that the increase plasma vitamin C of the subjects in this study is mainly due to improvement of the living condition of the population and widespread education of the people in the fundamentals of nutritional science in recent years.

此次用Farmer与Abt二氏微量测定血中维生素C的方法,前后测定了99名中学 生在一年四季血中该种维生素的含量,同时又以查账与秤重两种方法计算每人每日食物中维生素C的摄取量,借以观察两者之间的关系。结果发现由于不同食物中所供给维生素C的多寡与血中维生素C的含量有密切的关系。在冬季中,受检者血中维生素C的含量有显著的增加,而夏季则又有显著的降低,但在春秋之间并无显著的差别。再将此次所得的结果与过去国内外其他作者所报告的血中维生素C含量相比,则发现此次所得的结果较高,这可能是由于该校膳食改善的结果。从此次受检者血中维生素C的含量与齿龈健康情况检查的结果,很难看出两者之间有明显的关系。

Ⅰ. The Yinshan district as an example of "activizing region" in the Chinese platform One of the most typical localities that show clearly the phenomenon of"activization of platform" (активи. зация платформы) is the Yinshan region, aneast western mountain range on the border between the North-China plain andthe Mongolian plateau. It has long been recognized as a platform because ofthe presence of a folded foundation Pre-Sinian in age. However, owing to thefacts that Mesozoic crustal movements and magmatic activities...

Ⅰ. The Yinshan district as an example of "activizing region" in the Chinese platform One of the most typical localities that show clearly the phenomenon of"activization of platform" (активи. зация платформы) is the Yinshan region, aneast western mountain range on the border between the North-China plain andthe Mongolian plateau. It has long been recognized as a platform because ofthe presence of a folded foundation Pre-Sinian in age. However, owing to thefacts that Mesozoic crustal movements and magmatic activities are importantwithin this area, some geologists including G Schoenmann, hold that it is ageosynclinal region. It is Ю. М Шейманн who first noticed the phenomenon of activizationappearing in the Chinese platform. В. М. Синицын in his "Строенив и развитиекитайской платформы" indicates that some of the mountain ranges includingYinshan, which have been formerly referred to the folding belts developingfrom geosynclines, are in fact the internal structures of the Chinese platform. In this paper the writer after the opinion of В. М. Синицын, assigns theYinshan area as one of the "activizing regions" in the Chinese platform, andgives more detailed descriptions and discussions mainly on the point of thehistory of its stratigraphic development. Really it is a fact that the Yinshan region has an old folded foundationwhich is composed of metamorphic complex including chiefly gneisses, schists,and old granitic intrusions apparently Pre-Sinian in age. Since the formationof this folded foundation during the Luliang movement (=Goto-Karelian mo-vement), the old land of the Yinshan region has "activized" or "resurrected"several times. As early as in the Sinian period, a depression prolonging in E-Wdirection happened on its southern border, where Sinian limestone 900 metresin thickness and in some places up to 9,620 metres was so deposited. During a long time of the Palaeozoic era, the Yinshan old land was in the poriod ofdenudation except some Cambrian marine limestones only 144 metres in thick-ness deposited in the western part. At the end of the Palaeozoic era, local acti-vization with the formation of continental basin-deposits of Permian age, up to1,380 metres in thickness, as found in the Tachingshan area again happened.In the middle Mesozoic era, the Yinshan region came to a period of strongactivity. Structural depressions duo to "Процесс аркогенеза" occurred universallywithin the whole area and magmatie activities in large magnitude associatedthis crustal movement, so that a great sequence of freshwater basin-depositswith intercalations of volcanic beds, up to 8,000 metres in total thickness wereformed. During the formation of these strata, especially at the end of Mesozoic,interruptions of depositon happened frequently, folds and thrusts were abund-antly formed, and intrusive bodies of "young granite" were produced hereand there. In the Tertiary period, the Yinshan region was violently faulted, andvolcanic activities still happened, producing the basalt lava flow spreading ina wide area. The activity of the Yinshan old land has not ceased even to-dayas shown by the facte that its whole area is in the process of uplift and by thepresence of an earthquake zone known in the historical time. Ⅱ. To what Geotectonic Unit does the Southeastern Coastal Region of China Belong? On the Southeastern coast of China there is a district where geotectoniccharacteristics have never been recognized clearly. It is A. W. Grabau who firstreferred it to an old land named "Cathaysia". J. S. Lee holds the same opinion.In his geotectonic map of China, B. M. Синицын also assigns this region to aplatform and marks it as a part of his "Южно-китайский платформенный массив".However, there is still another opinion opposed to this. A. C. Хоминтовский, forinstance, renders recently this district to a geosynclinal region and proposes thename "Minche Pacific folding zone" for it. H. T. Yang and T. Y. Yu agreewith him. In the year 1954, the writer in his compilation-work connected with thegeology of Fukien and Kwangtung, found that the geotectonic characteristics ofthe southeastern coastal region of China are not only unagreeable with thosefound in a common platform on the one hand, but also contrasting, with thoseof a geosynclinal region on the other. In fact, it cannot be referred suitably toany geotectonic unit except to the intermediate type as shown by the history ofits geological development. Apparently it is an "activizing" or "resurrected" platform. During the Pre-Sinian crustal movement (the Luliang movement), a foldedfoundation composed of old gneisses, schists, and phyllites was completely for-med. Obviously this is a part of the broad old land of Southern China. In the earlier stage of the Palaeozoic era, the whole area of this region wasexposed in the air and under denudation. Hence, no deposit of any kind wasformed. After the Caledonian movement, depressions happened in the western partof this region, where the Devonian-Lower carboniferous continental deposit, theNanching series consisting mainly of quartzite, conglomerate and shale has beenformed, but the other parts were still under denudation. These facts show thatthis region was still a land at that time. Uralian and Lower Permian limestones, known respectively as the Chuan-shan limestone and the Chihsia limestone, separated from each other by adisconformity, spread widely in this region. This indicates that the marine trans-gressions really happened in the southeastern coastal region of China. However,the thicknesses of these limestones (only 30 metres and 150 metres respectively)and their uniformity in the horizontal direction show that the sea at thosetimes was shallow, and the magnitude of subsidence of the earth crust withinthis region was small. The unnoticed lateral changing of lithological charactersof these limestones proves the same fact. Undoubtedly these limestones arenothing but the marine deposits of platform-type. From Upper Permian toTriassic, this region was under a condition of alternation of transgression andregression of the sea. Owing to the fact that the amplitude of oscillation of theearth crust of this region at that time was small, the deposits formed duringthe marine transgression were thin and interrupted again and again by disconfor-mities (or even unconformities). Sometimes continental deposits are intercalated. Since the later period of Triassic, the southeastern coastal region has neverbeen covered by the sea again. And, a new condition began to happen in LowerJurassic. Here, the old land became to "resurrected", so that a series of depres-sing belts were formed as a result of "Процесс аркогенеза". In association withthe subsidence of these depressions, continental beds with a total thicknessup to 3,000 metres were deposited. In the beds interruptions frequently occurred.Folds were abundants, although they or at least some of them were intermediatetype. At the same time, magmatic activities were significant. Itappearedfirstly in the form of volcanic eruptions as recorded by a great sequence of beds consisting of tuff and rhyolite intercalating in the continental bedsmentioned above. And then, at the end of the Mesozoic, numerous graniticbodies were produced. Coming to the Cenozoic era, this region still sufferedfrom rather strong crustal movements accompanied by basalt lava eruptions. Theactivity of the old land has not yet been ceased even to-day as marked by thepresence of a famous earthquake zone between Kwangtung and Fukien, and theabundance of hot springs which widely spread within this region. All theseshow the typical characters of an "activizing" or "resurrected" platform. Final-ly, the complexity of the types of mineral deposits found in Fukien and Kwang-tung also proves the geotectonic nature of this region. Summarizing the whole matter, we may say that the southeastern coastalregion of China was originally an old land. Although it has been agian andagain submerged by the sea, the resulting marine deposits are entirely differentfrom those of geosynclinal region. In the middle of Mesozoic, this region beganto be active violently again, producing a series of depressions or "secondarygeosynclines", in which thick continental beds were deposited, and, at the sametime, folds of intermediate type, serious volcanic eruptions and magmatic intru-sions were produced. Hence, to refer the southeastern coastal region of China toan "activizing" platform is quite strongly proved. The northwestern boundary of this "activizing" platform is generally onthe line starting from central Chekiang through central Kiangsi to the Sou-thwestern part of Kwangtung, because the history and characteristics of geolo-gical development of the Southeastern Kiangsi and Central-southern Kwangtungare quite similar to those of Fukien and Eastern Kwangtung. As to the nomination of this geotectonic unit, the writer proposes to callit "Cathaysian activizing region". This name is derived from the "Cathaysia"of A. W. Grabau but adds, according to necessity, the meaning of activizing or"resurrected" characters of this region. The so-called "Minche Pacific foldingzone" of A. C. Хоминтовский is obviously unacceptable because it entirely doesnot coincide with fact. Compared with the "aetivizing" platforms found in other parts of theworld, the Cathaysian coastal "activizing" platform has its own characteristics,especially shown by the presence of numerous, widely spread, small depressionsor "secondary geosynclines", and the acidic magmatic activities appearing on alarge scale. All these indicate that this is a special type differing from all theknown "activizing

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