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The Dongtang Formation distributed in the Hengyang Basin of Hunan was named after Dongtang Village near the Xialiushi Station of Hengdong county (1964). It is composed of a sequence of purplish-red, light grey sandy mudstone, which lies between the underlying Daijiaping Formation (Upper Cretaceous) and the overlying Chashanao Member of the Xialiushi Formation (Late Palaeocene).The Dongtang Formation contains ostracods, charophytes,sporo-pollen and gastropod opercula, in which the ostracods are especially rich,...

The Dongtang Formation distributed in the Hengyang Basin of Hunan was named after Dongtang Village near the Xialiushi Station of Hengdong county (1964). It is composed of a sequence of purplish-red, light grey sandy mudstone, which lies between the underlying Daijiaping Formation (Upper Cretaceous) and the overlying Chashanao Member of the Xialiushi Formation (Late Palaeocene).The Dongtang Formation contains ostracods, charophytes,sporo-pollen and gastropod opercula, in which the ostracods are especially rich, including Cypridea (Morinina) nanxiongensis Guan, C. (M.) elongata Guan, C. (Pseudocypridina) rigida Guan, Porpocypris orbiculata Guan, Nanxiongium formosa (Guan), Sinocypris of. excelsa Guan, Eucypris dubia Guan and Darwinula sp., belonging to the Porpocypris orbiculata-Cypridea (Morinina) nanxiongesis-Parailyocypris taizhouensis assemblage. This assemblage is situated between the Talicypridea-Cypridea-Candona assemblage (Late Cretaceous) and Sinocypris excelsa-Parailyocypris chanzhouensis-Eucypris hengyangensis assemblage (Late Palaeocene), suggesting an Early—Middle Palaeocene age. It fundamentally corresponds to the Early—Middle Palaeocene Shanghu Formation assemblage in the Nanxiong Basin of Guangdong and resembles the Palaeocene ostracod fauna in the western United States.The charophtes and sporo-pollen are well correlated with the flora of the Shanghu Formation.The gastropod operculum, Mirolaminatus, is only distributed in the Lower Tertiary in Asia. and North America. Consequently, the Dongtang Formation can be assigned to the Palaeocene.In recent years, Late Cretaceous bivalves, sporo-pollen, dinosaur eggs and other fossils have been found to occur at the bottom of the so-called Dongtang Formation, and thus some authors assign this formation to the Late Cretaceous. Through research by the writer, it is proved the so-called Dongtang Formation bearing the above Late Cretaceous fossils should be of the Upper Cretaceous Daijiaping Formation.In short, 1. The age of the Dongtang Formation is Palaeocene.2. The Cretaceous—Tertiary boundary is put between the Daijiaping Formation and the Dongtang Formation.3. Owing to the difference in the sediment facies during the late Late Cretaceous, the upper part of the Daijiaping Formation consists of brownish-red and partly greyish-green siltstone, silty mudstone and mudstone in the middle part of the basin and of greyish-white, coarse- grained clastic rocks and greyish-green sandy mudstone near the margin of the basin, the latter rocks being wrongly regarded as the Dongtang Formation.

湖南衡阳盆地东塘组含有古新世的介形虫、孢粉、轮藻及早第三纪的腹足类口盖化石。介形虫属于早、中古新世组合,位于晚白垩世及晚古新世组合序列之间。近年报道的产于东塘组底部的晚白垩世双壳类、孢粉、恐龙蛋等化石,经观察皆赋存于上白垩统戴家坪组。从而证实,东塘组的地质时代为古新世,白垩系与第三系的界线在戴家坪组与东塘组之间。

Aperfect specimen of operculum has been found in Dalong Formation of Upper Permian in Lianyuan Huxingshan,Hunan. The operculum consists of one medial plate and two lateral plates and represents a new type named triapthychi.This paper indicates the fossil stratigraphic horizon and discusses the depositional environment,in which the operculum fossil was preserved.The shape of the operculum specimen is described and analysed in detail. It is inferred that this operculum is belong to a Hunanoceras. 2figs., 3refs....

Aperfect specimen of operculum has been found in Dalong Formation of Upper Permian in Lianyuan Huxingshan,Hunan. The operculum consists of one medial plate and two lateral plates and represents a new type named triapthychi.This paper indicates the fossil stratigraphic horizon and discusses the depositional environment,in which the operculum fossil was preserved.The shape of the operculum specimen is described and analysed in detail. It is inferred that this operculum is belong to a Hunanoceras. 2figs., 3refs.

涟源虎溪山发现的头足类口盖构造特殊,这种口盖由一块中板和两块侧板复合而成,代表一种新类型,命名为三分口盖。本文记录了化石的层位,分析了该化石层的沉积环境描述了口盖的形态并推断其为华南菊石的口盖。图2,参3。

A rapid and simple HPLC method was developed for the quantitative analysis of gliclazide in humanserum. After being extracted with benzene, gliclazide was analyzed by reversedphase HPLC colurnn (YWG-C(18)H(37)) and UV-detector(229nm) with tolbutamide as internal standard. The mobile phase was a mixture ofmethyl alcohol and 0.2%glacial acetic acid solution(5: 4 ) at a rate of 1mL/min. Over the concentrationrange of 0.25~32μmol/L, the linear regression equation was : Y=-0. 008412+0.1817X(n=8,r=0. 9996). The average...

A rapid and simple HPLC method was developed for the quantitative analysis of gliclazide in humanserum. After being extracted with benzene, gliclazide was analyzed by reversedphase HPLC colurnn (YWG-C(18)H(37)) and UV-detector(229nm) with tolbutamide as internal standard. The mobile phase was a mixture ofmethyl alcohol and 0.2%glacial acetic acid solution(5: 4 ) at a rate of 1mL/min. Over the concentrationrange of 0.25~32μmol/L, the linear regression equation was : Y=-0. 008412+0.1817X(n=8,r=0. 9996). The average recovery was 101.4%。 The average CV(n=5)for within day and betw-een day mea-surements were 2.9%and 4.1%respectively.

高效液相色谱法测定人血清中格列齐特胡玉钦,刘会臣,李新芳,朱光文(白求恩国际和平医院药理室石家庄050082)1前言格列齐特(gliclazide,GZ)系第二代磺酰脲类口眼降血糖药。为评价其片剂的生物利用度,本文建立了测定人血清中GZ的高效液相色谱...

 
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