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western hubei area
相关语句
  相似匹配句对
     ORDOVICIAN OSTRACODA FROM WESTERN HUBEI
     鄂西奥陶纪介形类
短句来源
     THE COMPOSITAE OF WESTERN HUBEI(Ⅰ)
     湖北西部菊科植物(Ⅰ)——斑鸠菊族、泽兰族、紫菀族
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     Western Blotting;
     western Blot; 地高辛标记的EMSA;
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     Western Australia
     展示澳大利亚西部净土
短句来源
     A RECOGNITION OF HYDROCARBON POTENTIAL IN WESTERN HUNAN AND HUBEI AREA
     湘鄂西地区油气前景探析
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According to the relation between relative sea level changes rates and reef growth rates,Permian reef in southern China can be devided into three types:offlapping reef,aggradational reef and progradational reef.When relative sea level rising rate is higher than reef growth rate,offlapping reef configuration was pingroduced.When relative sea level rising rate is equivalent to reef growth rate,aggradational reef configuration was formed.There are three types of progradational reef configuration:1) During relative...

According to the relation between relative sea level changes rates and reef growth rates,Permian reef in southern China can be devided into three types:offlapping reef,aggradational reef and progradational reef.When relative sea level rising rate is higher than reef growth rate,offlapping reef configuration was pingroduced.When relative sea level rising rate is equivalent to reef growth rate,aggradational reef configuration was formed.There are three types of progradational reef configuration:1) During relative sea level rising rate is lower than reef growth rate;2) Stillstand of relative sea level;3) relative sea level fall.Permian reef in southern China distributed mainly over Nanpanjiang area and eastern Sichuan to western Hubei area.There are the Maokou Age progradational reef and the Changxing Age aggradational reef in Nanpanjiang area.There are both offlapping reef and progradational reef of the Changxing Age in eastern Sichuan to western Hubei area. There are typical models of diagenetic and oil-gas pool in different types of reef. Firstly, relative sea level changes control on reef heterogeneous reservoir rocks and pore rich accumulation zone. Distribution of the time and space of petroleum in reef were controlled by reef heterogeneity. It is very important to recognize the regular patterns of the time and space of reef pore rich accumulation zone for exploration of the reef oil and gas pool. Secondly,relative sea level changes control on mechanism and configurations of the elements of the reef oil and gas bearing system.Analysis of the reef oil and gas-bearing system could help us preliminarily evaluate the potential of reef oil and gas-bearing system before drilling.Thirdly,different types of the reef complexes have their own contributing factors and regular patterns of the time and space.Through analysis of the contributing factors and regular patterns of the time and space ,we might predict buried reef more precisely.

根据相对海平面升降速率与礁生长速率之间的关系,中国南方二叠纪生物礁可划分为三种类型∶退积礁、并进礁和进积礁。不同类型的礁有其特有的成岩、成藏模式。首先,相对海平面升降控制了礁储集体的非均质性,这种非均质性又控制着原油在礁体内的时空展布,搞清这种时空展布规律对礁油气藏勘探极为重要;其次,相对海平面升降控制着礁含油气系统要素的形成机理及空间配置关系,对礁的含油气系统进行分析可在钻前对礁的含油气潜力作出初步评价。不同类型的礁体群均具有各自不同的成因联系及时空迁移规律,分析这种成因联系及时空迁移规律使我们可以更加准确预测潜伏礁体。

The genetic classification of organic reefs (prograded reefs, collateral reefs and retrograded reefs) is established from the angle of the control of the relative sea level rise and fall on the growth and development of reefs and the attributes of Permian reefs in the eastern Sichuan western Hubei area are described on that basis. The authors propose the view of co existence of prograded reef and retrograded reefs in the area and predict hidden reefs according to the directions of progradation...

The genetic classification of organic reefs (prograded reefs, collateral reefs and retrograded reefs) is established from the angle of the control of the relative sea level rise and fall on the growth and development of reefs and the attributes of Permian reefs in the eastern Sichuan western Hubei area are described on that basis. The authors propose the view of co existence of prograded reef and retrograded reefs in the area and predict hidden reefs according to the directions of progradation and retrogradation of reefs. They suggest that the horizon at the southeastern side of the Jiantianba reef cluster in western Hubei is equivalent to the hidden reef belt in the third member of the Changxing Formation, and that to the west of the Huaying eastern Sichuan reef forming belt there might exist a hidden reef belt which is stratigraphically equivalent to the top of the third member of the Changxing Formation.

从相对海平面升降对礁生长发育控制的角度建立新的生物礁成因分类 (进积礁、并进礁和退积礁 ) ,据此描述川东—鄂西地区二叠纪生物礁的属性 ,认为该区进积礁和退积礁并存。根据礁体的进积和退积方向对潜伏礁进行预测 ,指出鄂西地区见天坝礁群的东南侧应该存在层位相当于长兴组三段的潜伏礁带 ,华蓥山—川东成礁带以西可能存在层位相当于长兴组三段顶的潜伏礁带。

The internal quality and external appearance of 67 Ponkan (Citrus reticulata Blanco) fruit samples from main production areas of 9 provinces or municipality in 2001 and 2002 were analyzed. The results showed that the percentage of large(180.60 g±9.98 g), medium(151.24 g±7.48 g)and small(122.51 g±14.11 g)fruits is 42.9%,44.9% and 12.2% respectively; the average Brix of total samples is 12.5%±1.1% and the Brix of some samples collected from Rong county of Sichuan, Pinghe county of Fujian, Songzi county of...

The internal quality and external appearance of 67 Ponkan (Citrus reticulata Blanco) fruit samples from main production areas of 9 provinces or municipality in 2001 and 2002 were analyzed. The results showed that the percentage of large(180.60 g±9.98 g), medium(151.24 g±7.48 g)and small(122.51 g±14.11 g)fruits is 42.9%,44.9% and 12.2% respectively; the average Brix of total samples is 12.5%±1.1% and the Brix of some samples collected from Rong county of Sichuan, Pinghe county of Fujian, Songzi county of Hubei, etc. is less than 11.5%; the percentage of high(0.95%±0.10%), medium(0.69%±0.07%)and low(0.49%±0.07%) acidity is 22.4%、34.7%and 42.9% respectively. However, fruits from different production areas did not show significantly difference in peel color, Brix and vitamin C content. The fruit size from middle-southern Fujian province is nearly the same as that from southwest area of Sichuan province, but is significantly larger than those from areas of northern Fujian and Xuzhou, Lishui county of Zhejiang province, and western Hunan or western Hubei areas. There is no difference in acidity content between middle-southern Fujian and southwest Sichuan; both areas have lower acidity content than the other two areas. Additionally, the fruit from southwest area of Sichuan is significantly higher in the ratio of Brix/acid, and lower percentage of edible part than those from the rest three areas.

20 0 1和 2 0 0 2年对来自全国 9个省 (市 )主要产区的 6 7份柑品质进行了分析。结果表明 ,我国柑大 (180 6 0 g± 9 98g)、中 (15 1 2 4 g± 7 4 8g)、小 (12 2 5 1g± 14 11g)类型果实分别为 4 2 9% ,4 4 9%和 12 2 % ;分别有 6 1%和 4 4 9%的柑果皮颜色呈现黄绿或偏黄色和黄色 ;可溶性固形物平均含量为 12 5 %± 1 1% ,其中仅有四川荣县、福建平和和湖北松滋等部分地区柑可溶性固形物含量低于 11 5 % ;高酸 (0 95 %± 0 10 % )、中酸 (0 6 9%± 0 0 7% )和低酸 (0 4 9%± 0 0 7% )类型的果实比例分别为2 2 4 %、 34 7%和 4 2 9%。通过比较各柑主产区的主要品质指标发现 ,它们的果皮色泽 (a/b比值 )、可溶性固形物含量和维生素C含量没有明显差异 ;闽中南地区的果实明显重于闽北、浙江 (衢州、丽水 )和湘西鄂西地区的果实 ,而与川西南地区的差异不明显 ;闽中南地区和川西南地区的酸含量差异不明显 ,但...

20 0 1和 2 0 0 2年对来自全国 9个省 (市 )主要产区的 6 7份柑品质进行了分析。结果表明 ,我国柑大 (180 6 0 g± 9 98g)、中 (15 1 2 4 g± 7 4 8g)、小 (12 2 5 1g± 14 11g)类型果实分别为 4 2 9% ,4 4 9%和 12 2 % ;分别有 6 1%和 4 4 9%的柑果皮颜色呈现黄绿或偏黄色和黄色 ;可溶性固形物平均含量为 12 5 %± 1 1% ,其中仅有四川荣县、福建平和和湖北松滋等部分地区柑可溶性固形物含量低于 11 5 % ;高酸 (0 95 %± 0 10 % )、中酸 (0 6 9%± 0 0 7% )和低酸 (0 4 9%± 0 0 7% )类型的果实比例分别为2 2 4 %、 34 7%和 4 2 9%。通过比较各柑主产区的主要品质指标发现 ,它们的果皮色泽 (a/b比值 )、可溶性固形物含量和维生素C含量没有明显差异 ;闽中南地区的果实明显重于闽北、浙江 (衢州、丽水 )和湘西鄂西地区的果实 ,而与川西南地区的差异不明显 ;闽中南地区和川西南地区的酸含量差异不明显 ,但都明显低于另两个地区 ;另外 ,川西南地的区固酸比明显高于其他 3个地区 ,而可食率明显低于其他 3个地区。

 
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