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规模由
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  scale from
    family structure has changed from complex to simple and family scale from big to small;
    家庭结构由繁到减,家庭规模由大至小;
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  “规模由”译为未确定词的双语例句
    With the development of the market economy of our country, thefunction of familial firms is more and more remarkable day by day insociety and economy.
    随着我国市场经济的不断发展,家族企业在经济和社会中所起的作用日益显著,整体上呈现出规模由小到大、作用由弱变强、发展由慢变快的趋势。
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    The unit operation cost of the apparatus for water purification decreased from 2.575RMB/m3 to 0.717RMB/m3, when its scale of treatment increased from 10m3/d to 50m3/d.
    当该净水装置处理规模由10m3/d 增大到50m3/d 时,其单位运行费用由2.575 元/m3减小到0.717 元/m3。
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    But, Coase' s viewpoint isn' t right fully which the scale of the firm is the function of the cost of the firm' s organization and the cost of the market' s exchange.
    但科斯所说的企业的规模由企业的组织成本与市场的交易费用的比较来决定的观点是不完全正确的,应该是企业的组织成本与由此产生的低能激励成本之和与市场交易费用的比较。
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    After finishing the reforming of adaptability on reservoir engineering and production engineering,production capacity of reservoir increases gradually from 35×10 4 m 3/d to 70×10 4 m 3/d,and gas wells production is normal.
    完成气藏工程和采气工程适应性调整改造后 ,逐步将气藏开采规模由 35× 10 4m3 /d提升至 70× 10 4m3 /d左右 ,气藏气井生产正常。
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    the reserve scale of the oilfield is nine times that of the early days, productivity scale is increased to 19.0 10 t from the initial design of 2 . 5 10 t, and this number is still increasing.
    油田的储量规模增加到最初的9倍,产能规模由方案编制初期的2.5×104t增加到19.0×104t,并且仍在继续扩大。
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The surface relief on a scale from 10 nm to 100 μm showed a stochastic surface topography and revealed a hierarchy of grains.
      
Running mass ms at low scale from the heavy-light meson decay constants
      
What the so called short-range refers to the time scale from one month to one season or more.
      
Runoff likewise ranges in time scale from rapid surface terms to the slower base-flow.
      
The described circuit can be used for the time scale from 1 microsecond per division upward on an oscilloscope.
      
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Turbidity current deposits developed widely in Guizhou and Guangxi du-ring the Middle Triassic.Terrigenous materials came from island are in thesoutheast part of Guangxi,this is based on that:1.The turbidites in the south- east occured anterior to that in the northwest;2.The proximal facies in thesoutheast changes into distal facies in the northwest;3.Volcanic rocks decreasein thickness and even pinch out from southeast to northwest;4.The flow direc-tion of the flute castes point to NNE but not point to EW in...

Turbidity current deposits developed widely in Guizhou and Guangxi du-ring the Middle Triassic.Terrigenous materials came from island are in thesoutheast part of Guangxi,this is based on that:1.The turbidites in the south- east occured anterior to that in the northwest;2.The proximal facies in thesoutheast changes into distal facies in the northwest;3.Volcanic rocks decreasein thickness and even pinch out from southeast to northwest;4.The flow direc-tion of the flute castes point to NNE but not point to EW in the proximal facies;5.The scale of the flute castes changes gradually small from southeast to northwest.The quartz contentes are from 43 to 59%,SiO_2 ranges from 70.46 to72.04%,ratio of K_2O to Na_2O is less than 1 in the turbidite rocks,which isin accord with graywack of middle quartz content classified by Crook(1974),but it is in the range of high value.This shows that their formation condition maybe distent with oceanic crust but close to continental crust.In addition,the tur-bidity current deposits,ranging from 3000 to 5000 m in thickness throughoutthe study area,distributed extensively about 70000km~2 in Guizhou,Guangxiand Yunnan,which are bounded by a marginal reef barrier in the north and avolcanic island arc in the south.It is shown that such sediments were formedin back-arc basin but not fore-arc trench.It is because the turbidites belong to back-arc basin that the sediments con-tain intercalated beds of volcanic rocks.More over,the closer to the islandarc,the greater the thickness.Since the continental crust of the back-arc basinchanged thinner under the micro-spreading processes,mantle materials thus spil-led over to develop into basic,untrabasic intrusive bodies and slump conglo-merats that are resulted by faults.

黔、桂中三叠世浊流沉积的物源非西非东,而是来自桂东南岛弧,根据在于:(1)浊积岩的时代由东南向西北渐次变新;(2)东南发育近源相,西北发育远源相;(3)桂东南火山岩发育,近火山口特征明显,而桂西北却只有较薄的夹层,远火山口特征显著;(4)近源槽模 NNE 向,远源近于东西;(5)槽模规模由东南向西北明显变小。浊积岩石英含量43—59%,SiO 70.46—72.04,K_2O/Na_2O<1,正属于 Crook(1974)所划分的中等石英含量杂砂岩范畴,作为安第斯型大陆边缘海沟型的代表。其实,此一区间范围较广,应进一步细分,含量偏低者与洋壳关系密切,应属海沟型;偏高者与陆壳关系亲近,应属弧后盆地型。此区浊流沉积正属后者而非前者。广布70000km~2,厚达3000—5000m 的浊流沉积,北为边缘礁堤所限,南受火山岛弧所控,沉积物中既有中、酸性岩浆岩的踪迹,又有微型扩张地幔上溢的基性、超基性侵入岩体,正是弧后盆地的沉积特征。

There are Proterozoic and Mesozoic granites in Eastern Shandong. The Proterozoic Kunyushan granite belongs to the autochthonous—Parautochthonous one by metasomatism of the strata, the Jiaodong group, while the enormous amount of Mesozoic granites can generally be divided into three belts from west to east and follow the law below: from northwest to southeast, the eges of the granites become younger, the scale of magmatic activities increases, the acidity of the rocks increases and decreases, and increases again,...

There are Proterozoic and Mesozoic granites in Eastern Shandong. The Proterozoic Kunyushan granite belongs to the autochthonous—Parautochthonous one by metasomatism of the strata, the Jiaodong group, while the enormous amount of Mesozoic granites can generally be divided into three belts from west to east and follow the law below: from northwest to southeast, the eges of the granites become younger, the scale of magmatic activities increases, the acidity of the rocks increases and decreases, and increases again, and the rock bodies occur as stocks paralleling with each other, stretching in NE—direetion. The three granite belts are essentially parallel to the Benioff zone of the Pacific plate against the phitippine Sea plate, with the traction direction opposite to that of the plate movement. The granites of different ages in the region go.to the crustal remelting type,because they were formed through the intrusion of the rising granitic magmas as a result of the remelting of the pre-existing crustal rocks.

山东东部地区存在元古代和中生代花岗岩。元古代昆嵛山花岗岩是胶东群地层原地,半原地交代型花岗岩。大量的中生代花岗岩,由西向东大体上可分为三个带,并有如下规律:从西北向东南,时代由老变新,岩浆活动规模由小变大,岩石酸度由强变弱又变强,岩体都呈北东向互相平行的岩株状。三个花岗岩带与太平洋板块和菲律宾板块的毕鸟夫带大致平行。其推移方向与板块运动方向呈相反。各期次花岗岩的成岩作用,均是地壳先成的岩石重新熔化而形成的花岗岩浆上升侵入,故应属地壳重熔型(即S型)花岗岩。

After having done a series of investigations and researches of special topics on Lanzhou vegetable production-marketing development in resent years, the authors hold that the emphasis of the vegetable production for Lanzhou city should rest on"four transforms", i.e.vegetable varieties from few to more; its supplies from slack to thriving; its qualities from low to high; its scales from small to large.In order to have a comprehensive services and management for the vegetable production processing and marketing,...

After having done a series of investigations and researches of special topics on Lanzhou vegetable production-marketing development in resent years, the authors hold that the emphasis of the vegetable production for Lanzhou city should rest on"four transforms", i.e.vegetable varieties from few to more; its supplies from slack to thriving; its qualities from low to high; its scales from small to large.In order to have a comprehensive services and management for the vegetable production processing and marketing, the vegetable production and marketing group companies headed by state-owned vegetable corporations or other government functioned departments, that is the form of"market-company-peasant household", should be established.It is an effective measure and way to settle the problem of urban vegetable supply and demand contradictions.

笔者对兰州市近年蔬菜产销发展问题做了系列专题调查研究后认为,兰州市蔬菜生产的重点应实现“四个转变”:即品种由少变多;供应由淡变旺;质量由低变高;规模由小变大。并通过建立由国有蔬菜公司或其它职能部门牵头的蔬菜产销集团公司,即“市场+公司+农户”模式,对蔬菜的生产、加工、销售等进行综合服务和管理。这是一条解决城市蔬菜供需矛盾的有效途径。

 
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