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hard pressing
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  “hard pressing”译为未确定词的双语例句
     It is no doubt that it is a hard, pressing and actual task faced by Chinese oversea investing corporation to establish and consummate a whole set of human resource development and management system that is practical, high efficient, normative, and being in conformity with the international practice and the laws of the invested state.
     建立和完善一整套先进实用、高效规范、符合国际惯例和投资国法律的人力资源开发与管理体制,毫无疑问已成为中国石油海外投资企业所面临的一项艰巨而紧迫的现实任务。
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  相似匹配句对
     Design of Pressing Mould of the Hard Alloys Powder
     硬质合金粉末压制模具的设计
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     hard liver;
     肝脏质地坚硬;
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     Livelihood was hard;
     民生艰难,思想混乱。
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     Hard Ferrite Material with Hexagonal Structure Used for Dry-Pressing Production
     六角晶系干压取向用铁氧体永磁新材料
     Robot for Gemstone Pressing
     英研制成宝石加工机器人
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  hard pressing
One would thus expect that issues of taxation would not be as hard pressing as for other less endowed villages in the district.
      


A seismic reflection profile crossing the San Andreas fault zone in central California was conducted in 1978. Results are complicated by the extreme lateral heterogeneity and low velocities in the fault zone. Other evidence for severe lateral velocity change across the fault zone lies in hypocenter bias and nodal plane distortion for earthquakes on the fault. Conventional interpretation and processing methods for reflection data are hard-pressed in this situation. Using the inverse ray method of...

A seismic reflection profile crossing the San Andreas fault zone in central California was conducted in 1978. Results are complicated by the extreme lateral heterogeneity and low velocities in the fault zone. Other evidence for severe lateral velocity change across the fault zone lies in hypocenter bias and nodal plane distortion for earthquakes on the fault. Conventional interpretation and processing methods for reflection data are hard-pressed in this situation. Using the inverse ray method of May and Covey (1981), with an initial model derived from a variety of data and the impedance contrasts inferred from the true-amplitude stacked section, an iterative inversion process yields a velocity model which, while clearly non-unique, is consistent with the various lines of evidence on the fault zone structure.

1978年,在美国中加利福尼亚完成了一条横跨圣安德烈斯断层带的地震反射波剖面.由于断层带存在着强烈的侧向非均匀性和低速结构,观测结果极为复杂.这种断层带上的侧向速度急剧变化还有其它表征,诸如震中定位的偏移、地震节平面的变形等等.在这种情况下,处理反射波资料的常规计算与解释方法,已经难以实施.本文采用 May 和 Covey(1981)的射线反演方法,根据其它地球物理资料建立初始模型,再利用真实振幅的迭加剖面,推断出其阻抗对比的分布,通过反复迭代反演,获得了速度模型.反演计算的非唯一性固然存在,但该结果与断层带地区的各种地球物理证据是一致的,并揭示了圣安德烈斯断层带的细致结构.

At the present time two kinds of fossil ice margins have been found, con-gelifolds and fossils sand (loess) wedges in the strata of the studied area. The former is mainly found in the limnetic strata at the top of the Salawusu Group(Q31), The middle Chengchuan Group (Q32-2), The middle and the lower Dagouwan Group (Q43) and at the bottom of Dishaogouwan Group (Q43) along the Salawusu He in the southeastern depression Among them the middle Chengchuan Group is the largest and the widest.Besider, it can also be...

At the present time two kinds of fossil ice margins have been found, con-gelifolds and fossils sand (loess) wedges in the strata of the studied area. The former is mainly found in the limnetic strata at the top of the Salawusu Group(Q31), The middle Chengchuan Group (Q32-2), The middle and the lower Dagouwan Group (Q43) and at the bottom of Dishaogouwan Group (Q43) along the Salawusu He in the southeastern depression Among them the middle Chengchuan Group is the largest and the widest.Besider, it can also be found in certain horizons along the wuding He, Lu He, Hailuitu He, yulin He and Salawusu He near the loess hilly areas. The latter is mainly presented in the Tertiary mud stone or red earth, in the lower-middle Pleistocene loess or the lower part of the late Pleistocene sand (earth) gravel layer and on the top of the middle Chengchuan Group in the central-western dry denuded upland and the flat and lower areas on the low ridge land of its extending part to the depression.According to the morphological characteristics of the profile, these folds and wedges had not any relation to the genesis of tectonic movement fluvial-erosion, accumulation, glacier, mudflow, hard press of landslide and drying crack of ground surface, but to the stratum deformation or disturbance caused by seasonal nonhomogeneous melting and freezing processes for a long time in the frozen eartn area.The big or medium type of nondeveloped congeli-folds (mainly situated in the upper late pleistocene strata) and sand (loess) wedges(situated in the middle and lower profile)were related to the seasonal process of the permafrost and the other congelifolds located in the middle and lower Holocene strata and the small type of sand (loess) wedges located in the upper profile might possibly be formed under the condition of the deep seasonal frozen earth and even the other year's frozen earth.According to the relation of the phenomenon of fossil ice margins with the existing horizon and the physterogenetic or contemporaneous association of over-rlying eolian sand or loess, and referring to the measured data of absolute age of the strata concerned, it is roughly determined that the congelifolds on the top of the Salawusu Group, in the middle Chengchuan Group, the middle and lower Dagouwan Groop and at the bottom of Dishaogouwan Group were formed at the early and late sections of the late stage of the late pleistocene of 70,000 and 25,000 years B.P.and the mid-late stage and at the beginning of the late stage of the Holocene of 5000 years or 3200 years and 2300 years B.P.respectively, the situation of sand (loess) wedges was very similar to the above-mentioned situation.These periods correspond to the early Yumu glacial epoch, the late Yumu glacial epoch and the beginning of new glacial epoch and the small glacial epoch.It shows that during these periods the studied area was influenced by the fluctuation of cold weather of the four glacial epochs of the Northern Hemisphere.The above-mentioned data of fossil ice margins have provided new reliable evidences for the reconstruction of the ancient climatic environment, the division of climatic strata, the comparison and the prode in the genesis in the study area since late pleistocene.The study suggests that the study area at the early and late sections of the late stage of late pleistocene and the mid and late Holocene or late Holocene was island-like permafrost and deep seasonal frozen earth or the other yearxs frozen earth area at the southern periphery of the continuous permafrost zone,the climate then was generally dry and cold and there was much northwest wind;eolian sand or loess and the deposition of fluviolacustrine facies or fossil soil belonged to the products of dry and cold ice margins or near ice margin environment and warm wet non-ice margin environment respectively, since late pleistocene the study area had undergonemany times of climatic fluctuation of the replacement of ice margin of warm wet facies with that of dry cold facies.The main cause was that the study area was situated in the transitional

本文概述了鄂尔多斯高第三系至全新统地层中融冻(衤习)皱和沙(土)楔两类古冰縁现象的分布与形态特征,探索了它们的成因以及同所在地层和上覆风成沙或黄土的关系,並对古冰縁现象的气候地层学意义作了讨论。

This paper studied behaviour type of 100 cases with rheumatic heart dsease,48 cases with coronary heart disease and 60 normal persons by means of four different investigation methods.Results showed that A type of behaviour ratio in rheumatic heart dis- ease.and coronary heart disease distinctly higher than normal persons contrast group.(The percentages separetely were 71%、56.2%,P<0.001 and P<0.01).Results of daily life in- vestigation list same showed that value over normal upper limit(>60.2)in rheumatic heart...

This paper studied behaviour type of 100 cases with rheumatic heart dsease,48 cases with coronary heart disease and 60 normal persons by means of four different investigation methods.Results showed that A type of behaviour ratio in rheumatic heart dis- ease.and coronary heart disease distinctly higher than normal persons contrast group.(The percentages separetely were 71%、56.2%,P<0.001 and P<0.01).Results of daily life in- vestigation list same showed that value over normal upper limit(>60.2)in rheumatic heart disease was distinctly higher than normal person group(P<0.05).Jenkin's list showed per- centage of rheumatic heart disease group was higher than normal person group(P<0.05), Alexithymia list abnormal in rheumatic heart disease was higher than normal person group, but no statistical importance(P>0.05). In the contrast research of patients with heavy pathological changes,bivalve replacement (BVR)and with light pathological change,mono—valve replcement(MVR),in various ques- tions and answers,integral value of contending for strongnes and seeking to do others down. hostility and easily anger,showed that value of BVR was higher than value of MVR(P<0. 01),but time hardpressing(TH)and total integral value both never showed difference. This result preliminarily suggested that A type behaviour not only was important risk factor of coronary heart disease attack,but also may be relating to pathogenity action and curing the sickness action in developemental process of rheumatic heart disease.This remained to be confirned by hereafter further research.

本文运用四种不同调查方法研究了100例风心病、48例冠心病和60例正常人的行为类型。其结果显示:风心病和冠心病A型行为比例明显高于正常对照组(其比例分别为71%、56.2%、P<0.001和P<0.01)。日常生活调查表结果同样显示出风心病超正常上限(>60.2)者,明显多于正常组(P<0.05),Jenkin's表显示风心病组其百分率高于正常组(P<0.05),Alexithymia表不正常者风心病组虽高于正常组,但无统计意义(P>0.05)。病变重,行双瓣替换术(BVR)和病变较轻行单瓣替换术患者(MVR)比较研究中,各类问卷中的争强好胜、敌意和易怒(CH)一项积分值显示双瓣替换术者高于单瓣替换者(P<0.01)而时间紧迫感(TH)及总积分值,二者均未显示有差异。这一结果初步提示:A型行为不仅是冠心病发病的重要危险因子,亦可能与风心病发展变化过程中的致病和治病作用有关。这一点有待今后进一步研究证实。

 
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