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扬子
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  yangtze
     By estimating the movement velocities of these stations and using a least-square fit under the hypothesis of a rigid body, the modern velocities of the Sichuan-Yunnan, Sichuan-Qinghai and Yangtze block movements are 19.2±2.8 mm/a, 10.7±3.2 mm/a and 9.7±1.6 mm/a respectively and the direction of their movement changes from SE to ESE gradually, indicating the features of clockwise vortex.
     利用所得的运动速度结果,采用刚性地块假设下的最小二乘法拟合方法,得到川滇、川青、扬子地块运动速度分别为(19.2±2.8)mm/a、(10.7±3.2)mm/a、(9.7±1.6)mm/a,地块运动方向由SE逐渐变成SEE,呈现出顺时针旋卷特征;
短句来源
     After forming of metamorphic recrystallization of basement(Ar-Pt_1):1.the stage of "open"and "close" between the plates of North china and Yangtze(Z-D_2),including the stage of Craton-passive-continental margin(Z-O_2)and global uplift-(back-arc) basin(O_3-D_2);
     在变质结晶基底的形成(Ar-Pt_1)之后:一、华北板块与扬子板块“开”“合”阶段(Z-D_2),包括克拉通—被动大陆边缘盆地阶段(Z-O_2)和整体隆升—弧后盆地阶段(O_3-D_2);
短句来源
     The U-Pb ages of zircon concentrate in 1500~1900Ma,700~900Ma、200~400Ma,consistent with magmatism activities in Yangtze block and southern Qinling.
     锆石的U-Pb年龄集中分布于1500~1900Ma、700~900Ma、200~400Ma,与扬子地块、南秦岭的岩浆活动相一致。
短句来源
     In the northern margin of Yangtze Plate, there are 4 types of prototype basin, the passive continental edge basin (Pt_3-O), the peripheral foreland basin (D-C), the aulacogen basin (P-T), and the intracontinental foreland basin (T_3-K_1).
     扬子北缘有4套性质不同的原型盆地,即被动大陆边缘盆地(Pt3-O),周缘前陆盆地(D-C)、拗拉槽盆地(P-T),陆内前陆盆地(T3-K1)。
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     Application of MPC system in 20000m~3/h air separation plant operating in Yangtze Petrochemical Company
     MPC在扬子20000m~3/h空分设备中的应用
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  “扬子”译为未确定词的双语例句
     The optimization of hydrorefining process condition after YPC-PTA plant modification are discussed,the main process parameters are determined,the reaction pressure is 7.0~7.25 MPa,the reaction temperature is 282~283 ℃,the compounding concentration is 27%~28%,the catalyst quantity is 10 500 ~11 000 kg.
     对扬子PTA装置改造后加氢精制工艺条件的优化进行了探讨,确定了主要工艺参数:反应压力7.0~7.25MPa,反应温度282~283℃,配料质量分数27%~28%,催化剂充填量10500~11000kg。
短句来源
     And the sequence classification and regional correlation of Carboniferous in Lower Yangtse area are discussed. Results show that this area can be divided into 6 third,grade sequences (SQ1-SQ6),among which SQ1,SQ5,SQ6 belong to Type Ⅰ sequence; SQ2,SQ3,SQ4 to Type Ⅱ sequence.
     研究结果表明,苏皖下扬子地区石炭系可以分为6个三级层序,其中层序SQ1、SQ5、SQ6属于Ⅰ型层序,层序SQ2、SQ3、SQ4属于Ⅱ型层序。
短句来源
     The AcOH consumption of PTA Plant in Yangzi Petrochemical Co. experienced the course from 100 kg/t,68 kg/t to 54 kg/t.
     扬子石化PTA装置的醋酸消耗经历了从100kg/t—68kg/t—54kg/t的历程。
短句来源
     The feasibility of making further improvement on the production capacity of Yangzi Petrochemical Co PTA plant on the design basis of 600 kt/a modification was analyzed.
     分析了扬子石化公司PTA装置在600kt/a改造的设计基础上,进一步提高生产能力的可行性。
短句来源
     The study area is located in the east of changjiangriver in East China Sea(30.7o~32.6oN、122.5o~125oE),which water deep 30~50m and an area of 3×104sqmeters.
     本文所研究的扬子浅滩位于内陆架外缘长江口东侧30.7o~32.6oN、122.5o~125oE处,水深30~50米,总面积约3万km2。
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     The author considers that there arethree subspecies of Neophocaena phocaenoides existing in the Chinese waters, thatis, N.
     亚种N.
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     Revamping-expansion project of ethylene plant in Yangzi Petrochemical Corporation
     乙烯改扩建工程
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  yangtze
Affecting factors of preferential flow in the forest of the Three Gorges area, Yangtze River
      
In order to study the factors affecting preferential flow, a 2.9 m-long, 2.6 m-deep soil profile was dug in the Quxi watershed, Yangtze River.
      
Particularly, rugose coral fauna of the Sifengya Formation represent early Telychian rugosan fauna in the Upper Yangtze region and improve the sequences of early Silurian (Llandovery) rugose coral assemblages in Yangtze region.
      
In this study, thirty-six individuals of Acheilognathus macropterus were collected from the Heilongjiang River, the Yangtze River, and the Nandujiang River.
      
The samples from the Yangtze River scattered into clades 2, 3, and 4.
      
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本文在綜合研究宁鎮山脈象山羣岩层縐构造形态基本特征、分布規律和形成机理的基础上,专門論述了海西印支裡縐构造的基底断裂如何控制燕山盖层褶縐形成的具体表現方式,論証了燕山运动以块断运动为主的构造性貭,为进一步研究下揚子地区岩漿活动和成矿作用的空間分布規律提供了构造方面的依据。

The Hsuehfeng cycle of the region under discussion is taken as a stage of eugeosynclinal development. The eugeosytnclinal formational sequences are rich in volcanic rocks which have been folded into tight linear folds by the Hsuehfeng movement. The Hsuehfeng folded belt is responsible for the formation of the Kiangnan geanticline of the Caledonian cycle. The South Anhui geosyncline extends along the northern side of the Kiangnan geanticline and is filled with the miogeosynclinal formational sequences which have...

The Hsuehfeng cycle of the region under discussion is taken as a stage of eugeosynclinal development. The eugeosytnclinal formational sequences are rich in volcanic rocks which have been folded into tight linear folds by the Hsuehfeng movement. The Hsuehfeng folded belt is responsible for the formation of the Kiangnan geanticline of the Caledonian cycle. The South Anhui geosyncline extends along the northern side of the Kiangnan geanticline and is filled with the miogeosynclinal formational sequences which have vast thickness of more than ten thousand meters and consist of typical geosynclinal formations (flysch formation, graywacke formation, siliceous shale formation, etc.) with zonal arrangement. The geometric styles of folding in the South Anhui geosyncline are of linear complex folds the individual fold of which is either tight or open in form, which indicates the varied origin of the folded structure. On the basis of the above mentioned structural characteristics it is to be compared with the West Chekiang Caledonian geosyncline, Through comparative research and analysis of the South Anhui, Northwest Kiangsi and West Hunan Caledonian geosynclines bondering the northern side of the Kiangnan geanticline, the present writer has found that their similarities are rather obvious. Thus they form as a whole the belt of the marginal geosynclinal depressions. The South Anhui Caledonian geosyncline could be distinguished from the South Kiangsi Caledonian inner geosyncline by the following diagnostic features: (1) it has more abundant carbonate rocks in the sedimentary sequences; (2) it possesses comparatively open style of folding; (3) the trough of sedimentation migrates from the Kiangnan geanticline towards the platform throughout the early palaeozoic period; and (4) it displays weak regional metamorphism and igneous activity. Judging from the above-stated reasons, it is less mobile and displays the character of a residual geosyncline. The Shitai-Guogongtzang deep fault marks the boundary between the South Anhui Caledonian geosyncline in the south and the Lower Yangtze Pericratonic Subsidence zone, having the carbonate formation of platform type, in the north. During the Caledonian cycle the Nantian trough is superimposed upon the eastern part of the Kiangnan geanticline and distinguished from the South Anhui geosyncline by the incompleteuess of the sedimentary cycle, its paramolasse formation and the basin-shaped syncline. The Kiangnan geanticline broadly controls the formational and structural development of the South Anhui geosyncline and the West Chekiang geosyncline on both sides. Thus the South Anhui geosyncline together with the West Chekiang geosyncline and the Kiangnan geanticline constitutes a geosynclinal system which forms the northeastern section of the South China Caledonian geosynclinal region.

皖南南部构造性质及构造单元的归属的争论,在最近一次全国性编图会议,意见仍未统一。作者在实际调查材料的基础上,运用构造——建造分析和比较大地构造的方法研究了本区前寒武纪及早期古生代各时代建造成分,确定了各建造的名称、性质和空间分布特征,进一步划分出几个不同性质的建造序列;描述了不同时代地层和不同空间的构造形态,划分了构造层及构造形态的级别,並分析了构造形态形成的原因;论证了本区加里东运动的存在及其性质。在上述资料基础上,阐明了本区是华南加里东地槽区皖南浙西加里东地槽系的重要组成部分,並对皖南加里东地槽与其北隣的下扬子台缘沉陷带的界限予以确定,进一步说明了本区在加里东旋迴是冒地槽,具有残余地槽和边缘地槽拗陷的特性。

This paper aims at giving an account of the distribution of the Ordovician sedi-ments in North China,with brief reference to fossil zones and chronological relation-ship of nautiloids to graptolites and other invertebrate fossils.The history of sedimen-tary development and the distribution of the Polydesmia fauna indicate the fact thatin the Beianzhuang age immense marine water rapidly transgressed the Yellow Riverrealm and also spread over a vast land of Gan-Qing-Zang realm.One of the remar-kable events in...

This paper aims at giving an account of the distribution of the Ordovician sedi-ments in North China,with brief reference to fossil zones and chronological relation-ship of nautiloids to graptolites and other invertebrate fossils.The history of sedimen-tary development and the distribution of the Polydesmia fauna indicate the fact thatin the Beianzhuang age immense marine water rapidly transgressed the Yellow Riverrealm and also spread over a vast land of Gan-Qing-Zang realm.One of the remar-kable events in the Beianzhuang age is that numerous actinoceroids made their firstappearance.The actinoceroid fauna has relations with those in Australia and NorthAmerica.A brief discussion is also made on the correlation of the Yellow River realm,the correlation of North China to South China and the wide distribution of the YellowRiver type,which,together with the Yangtze River type and the Pearl River type,constitutes three principal bio-sedimentary types in China and may be more or less usedas an approach to the analysis of bio-sedimentary provinces of the world.The bio-sedimentary provinces are controlled distributionally by the paleo-tectonic factor and bythe palaeolatitude,with Central Pacific and Northwest Africa as the North Pole andthe South Pole respectively.The Yellow River type was in the low latitudinal area;its distributional discontinuity may be related,in paleotectonic sense,to the stable shal-low sea.The Yangtze River type,equivalent to the Baltic one,ranged a little lower inthe middle latitudinal area and in the sub-stable shallow sea.The Pearl River type,cor-responding to the British one,was in the middle latitudinal area and in the mobileisland arc.

本文描述了头足类化石29种,分属于25属、19科、1亚科、19科,其中24新种、6新属、1新科。对我国北方奥陶纪地层划分进行了详细讨论,将我国奥陶纪地层按生物-沉积特征划分为珠江、扬子、黄河三种类型及珠江、扬子、黄河、新疆、甘青藏和大兴安岭六个生物-沉积区。将黄河区奥陶纪地层划分为下奥陶统冶里组、亮家山组、北庵庄组、马家沟组和中奥陶统阁庄组、八陡组,并和国内外相当的地层进行了对比。

 
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