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the primary nature
相关语句
  原生自然
     The primary nature is the one existing as it was, providing mankind with survival environment and resources.
     原生自然是指原本存在的自然,供给人生存条件和资源,二者存在供需关系。
短句来源
     The primary nature's supply to mankind and its capacity of mankind's supply are unlimited, where the supply-demand relation may completely be adjusted by markets.
     原生自然对人类的供给和容纳人类的供给是无限的,供需完全可由市场调节。
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  “the primary nature”译为未确定词的双语例句
     This paper gives an analysis on the abundance of the organic matter with an emphasis on the interrelationship between the primary nature of the organic matter and the depositional phases taking these factors as early diageuesis,low abundance of organic matter,having been migration channel and reservoir rock of the interference of outside organic matters etc.
     本文针对碳酸盐岩成岩早,有机质丰度普遍低,曾经是输导层、储集层,有外源有机质干扰等问题,着重从有机质的原生性及其与沉积相的制约关系进行了论证。
短句来源
     Conclusions: It's feasible to study the MDR1 expression of malignant solid tumors and helpful to recognize the primary nature of multidrug resistance and has important clinical significance for chemotherapy.
     结论:研究恶性实体肿瘤细胞MDR1表达是可行的,可明确其原始的药物敏感性,对临床化疗有重要价值
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  相似匹配句对
     Primary hypophysitis
     原发性垂体炎
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     Will is primary.
     意志是第一性的,理性则是由意志派生出来的,理性命定为意志服务。
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     Primary Education of the U.S.
     我所看到的美国小学教育
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     The primary conclusions are:
     主要结论如下:
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     On the Nature of History
     略论历史的本质——从认识论的角度谈历史
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  the primary nature
The primary nature of the Be evolution strongly suggests that supernova ejecta are the sources of this material.
      
Both data sets pass the inclination-only fold test, demonstrating the primary nature of these magnetisations.
      
Leukocytes of the parents exhibited intermediate activities, which suggests the primary nature of β-galactosidase deficiency.
      
It is suggested that esophageal melanocytosis as well as the presence of junctional changes may determine the primary nature of malignant melanoma of the esophagus.
      
Relatively iron-rich lherzolite xenoliths of the Cr-diopside suite: A guide to the primary nature of anorogenic tholeiitic andes
      
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After studying the depositional organic matters of Late Cenozoics in Kun- ming basin, the typical inland fresh water lake basin in China, some results and recognitions have been found as follows. 1. The primary nature and character of depositional organic matter, and its original transform in the early diagenesis stage have been revealed by stu- dying the modern deposit sapropel (ZK_2, shallow drilling hole) and late Cenozoic sediments (Dian ke hole-1 and CAN hole-3) of Dianchi in Kunming basin. It is...

After studying the depositional organic matters of Late Cenozoics in Kun- ming basin, the typical inland fresh water lake basin in China, some results and recognitions have been found as follows. 1. The primary nature and character of depositional organic matter, and its original transform in the early diagenesis stage have been revealed by stu- dying the modern deposit sapropel (ZK_2, shallow drilling hole) and late Cenozoic sediments (Dian ke hole-1 and CAN hole-3) of Dianchi in Kunming basin. It is helpful for representing the accumulation, transform and the general model for the generating hydrocarbon original stage of the depositional organic matters in the inland lake basin; tracking back to the composition, texture and property of organic matter in the early diagenesis stage of the fresh wa- ter deposit of the inland lake basin. It is possible to determine the marks of continenial organic parent matter in order to track original organisms. The original transform of organic matter while R_0<0.3% is quite favorable for discussing the relationship between the early diagensis stage and the early transfrom of organic matter. No doubt, it is very important to perfect and substantate the mechanism of generating hydrocarbon in the contintal facies. 2. The research results can prove that the organic matters are quite ab- undant with may kinds of natural organism types, formed by various types of the parent matter, but the type Ⅱ and Ⅲ are still the majority in the in- land fresh water lake basin. 3. The research results can also prove that the weak transform of depo- sitional organic matters is present under the condition that the depth is less than 500m, Ro is less than 0.3% and the geotempreture is less than 50℃, and the limited heating is not the only factor which plays a determining role, but it is a result of multiple influences.

本文以我国典型内陆淡水湖盆——昆明盆地晚新生代沉积有机质的基础研究为依据,探讨内陆淡水湖盆沉积有机质的主要组成——可溶有机质,不溶有机质(干酪根),腐殖物质及氨基化合物等的原生特征及其在早期成岩阶段的演化,力图探索广泛赋存于内陆淡水湖盆沉积中的有机生源物的特征及相应判别标志,探索并再现早期成岩作用与有机生源物早期演化的对应及相互依存制约关系,以期逐步完善并充实陆相成烃模式。

This paper gives an analysis on the abundance of the organic matter with an emphasis on the interrelationship between the primary nature of the organic matter and the depositional phases taking these factors as early diageuesis,low abundance of organic matter,having been migration channel and reservoir rock of the interference of outside organic matters etc.It is believed that the carbonate source rock should have a certain abundance of organic matter and these organic matters is primary in nature.They...

This paper gives an analysis on the abundance of the organic matter with an emphasis on the interrelationship between the primary nature of the organic matter and the depositional phases taking these factors as early diageuesis,low abundance of organic matter,having been migration channel and reservoir rock of the interference of outside organic matters etc.It is believed that the carbonate source rock should have a certain abundance of organic matter and these organic matters is primary in nature.They are governed strongly by the sedimentary phases.The abundance is affected obv- iously by lithology,color,acid insolubles etc.They are appraised by a clas- sification according to the value of C%:<0.2,0.2-0.35,0.35-0.5 and>0.5.

本文针对碳酸盐岩成岩早,有机质丰度普遍低,曾经是输导层、储集层,有外源有机质干扰等问题,着重从有机质的原生性及其与沉积相的制约关系进行了论证。认为碳酸盐烃源岩应具备原生性,具有一定的丰度值,它们密切受沉积相的控制;在相似相带下,丰度值受岩性、颜色、酸不溶物等因素的影响明显。最后提出按 C%=<0.2;0.2—0.35;0.35—0.5;>0.5进行四级评价。

We collected 262 samples at 39 sites in three thick Lower Permian sections along the northwestern margin of the Tarim basin.The Lower Permian sections are composed of basalts interbedded with limestones or sandstones, or shallow marine limestones and sandstones alone, all with good biostratigraphic age control. Alternating field(AF)and thermal demagnetization experiments remove small secondary effects and reveal stable, characteristic magnetizations. Reversed directions ( consistent with the Kiaman Reversed...

We collected 262 samples at 39 sites in three thick Lower Permian sections along the northwestern margin of the Tarim basin.The Lower Permian sections are composed of basalts interbedded with limestones or sandstones, or shallow marine limestones and sandstones alone, all with good biostratigraphic age control. Alternating field(AF)and thermal demagnetization experiments remove small secondary effects and reveal stable, characteristic magnetizations. Reversed directions ( consistent with the Kiaman Reversed Interval) . similar directions between basalts, sandstones and limestones,and a positive fold test all attest to the primary nature of the remanence. Two paleomagnetic poles, one from the limestone section (A=65° N, φ=163° E, K=128, A35 = 4° n=11 sites) and the other from the two basalt sections ( A = 55° N, φ=172° E, K=66, A55=4°, n=21 sites) . are obtained. Combined with previous published data ( Bai et al., 1985; Li, 1988), a Permian paleomagnetic pole(φ=61°N. φ=177° E, K = 98, A55 = 9°, N = 4 studies ) is given for the Tarim block. The permian paleolatitude of the Tarim block was much higher than those of the Si no-Korean and Yangtze blocks, suggesting it's independence from the others. Significant post-Permian relative motion have occurred between the Tarim, Siberian, Sino-Korean and Yangtze blocks, hence,a geologically inferred Late Paleozoic amalgamation was juts the beginning in the complex tectonic evolution of Central and Eastern Asia.

在塔里木盆地西北缘下二叠统的三个剖面中采集的标本,获得了两个古地磁极:一个获自灰岩剖面(λ=65°N,φ=163°E,K=128,A_(?5)=4°,n=11).另一个获自两个玄武岩剖面(λ=55°N,φ=172°E,K=66,A_(95)=4°,n=21).结合原先已发表的数据,塔里木地块二叠纪古地磁场为λ=61°N,φ=177°E.K=98.A_(95)=9°,N=4.塔里木地块古纬度比中朝、扬子地块高得多,认为这些地块是分开的大陆地块.晚二叠世.塔里木、西伯利亚、中朝、扬子地块之间发生过重要的相对运动表明.地质上推断的晚古生代碰撞、并合作用在中亚及东亚的复合构造演变才刚刚开始.

 
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