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strong stress     
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  强应力
     Otherwise,Al~(3+),K~+,Ti~(4+),Na~+ and Ca~(2+) were abundant in weak stress zones,but Si~(4+),P~(5+),Fe~(2+)+Fe~(3+) and Mg~(2+) abundant in strong stress zones.
     在弱应力带富集Al3+、K+、Ti4+、Na+、Ca2+; 在强应力带富集Si4+、P5+、Fe2++Fe3+、Mg2+。
短句来源
     When rock suffers from strong stress, it produces ductile deformation which microcosmically appears dislocation.
     岩石在强应力作用下产生屈服 (韧性形变), 微观上表现为位错。
短句来源
     The strong stress sensibility is evidenced by the laboratory data of confined pressure core porosity and core permeability relationships.
     室内岩心围压 孔隙度、围压 渗透率关系数据证实了两油藏储层的强应力敏感性。
短句来源
     Queries to the viewpoint low permeability reservoirs have not the characteristics of strong stress sensitivity.
     对“低渗透储层不存在强应力敏感”观点的质疑
短句来源
     The metallogenic model of alluvial type gold placer is put forward by the author in this paper,according to analysis on the formation process of gold placer. It is considered that gold placer gets into sedimentary basin together with gravel and sand by strong stress,such as water,during the process of downgoing of local earth crust.
     本文通过对砂金矿床形成过程的分析认为:在地壳局部下沉过程中,砂金在水等强应力作用下,与砾石、砂一起进入沉积盆地,形成砂金的中间储存体;
短句来源
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  强胁迫力
     STRONG STRESS TRIGGERS CATASTROPHIC CHANGE ON FRAGILE ENVIRONMENT: AN EXAMPLE OF THE DEVELOPMENT HISTORY FOR THE PAST 100 YEARS IN THE SONGLIAO PLAIN
     强胁迫力使脆弱环境突变——松辽平原百年开发史例证
短句来源
  较大的应力
     The causes of the cracks in the cast iron mold used for casting aluminum were studied by analyzing macrostructure and microstructure. The results show that the cause of the cracks is that the mould was made of pearlite grey iron,strong stress could be created by the expand and cooling shrinkage when pouring 720 ℃ aluminum;
     针对铸铝用铸铁模具在使用过程中产生裂纹问题,经分析表明:产生裂纹的原因是原铝锭铸铁型是由以珠光体为基的普通灰口铸铁制造,在浇注720℃铝液时,由于热胀冷缩将产生较大的应力;
短句来源
  “strong stress”译为未确定词的双语例句
     Strong stress in response to restraint was observed in rats. In these rats, plasma ACTH increased significantly (P<0.001) while T_3 and T_4 decreased (P<0.05).
     实验观察到束缚可使大鼠产生严重的应激,表现为血浆促肾上腺皮质激素(ACTH)上升(P<0.001),甲状腺素(T_4)和三碘甲状腺素(T_3)下降(P<0.05)。
短句来源
     The fluids then migrated into the middle basin along J/T and O/C unconformities or cracks by strong stress.
     这些流体在构造应力作用下主要沿J/T、O/C不整合面运移至盆地中部。
短句来源
     Three treatments of control,light stress,strong stress (osmotic potential of culture solution was 0 0,-0 1,-0 3 MPa, respectively) were set up in water cultivation system in greenhouse of Okayama University in Japan.
     室内干旱胁迫处理是将臭柏插穗带往日本冈山大学扦插 ,生根扦插苗移植于砾耕栽培装置中 ,设置对照区、弱干旱胁迫区、强干旱胁迫区 (培养液渗透势分别为 0 0、- 0 1、- 0 3MPa) 3种处理进行长期干旱胁迫室内模拟试验。
短句来源
     In Okayama University of Japan,longterm simulation experiment in greehouse are conducted with three different treatments:control,light stress,strong stress in water culture systems,in which concentrations of solutions are 0 MPa,-01 MPa and -03 MPa respectively.
     室内实验是将臭柏插穗带往日本冈山大学扦插,生根扦插苗移植于砾耕栽培装置中,设置对照区、弱干旱胁迫区和强干旱胁迫区(培养液渗透势分别为0MPa、-0 1MPa和-0 3MPa)3种处理进行长期的干旱胁迫室内模拟实验。
短句来源
     Strong stress sensitivity is an important character of fractured reservoirs and will affect exploitation project.
     较强的应力敏感性是裂缝性储层的重要特征之一,并直接关系到裂缝性储层开采方案的制定。
短句来源
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  strong stress
However, our model shows that strong stress fluctuations may be an immediate precursor of catastrophic failure statistically.
      
Due to this pre-slip, strong stress concentration has developed around the pre-slip area and a dynamic rupture starts at a certain point on the rim of the pre-slip region.
      
They showed a strong stress history dependence as has already been observed for αk in several crystalline rocks.
      
In case of weak and strong stress the model has to be used with some precautions.
      
These structural defects possess strong stress fields and directly adjoin grain boundaries.
      
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The thyroid hormone levels in 55 patients with epidemic hemorrhagic fever(EHF)were dynamically analysed during the whole course of the disease.The result showed that all patients had increased serum TSH levels at each phase in the course of the disease and the values of serum TSH in the mild group were higher than in those of the severe group. In most cases,the concentration of total serum T_4(TT_4)was significantly decreased(6.2± 3.69μg/dl)at the critical stage of the disease.The mean serum T_3 concentration...

The thyroid hormone levels in 55 patients with epidemic hemorrhagic fever(EHF)were dynamically analysed during the whole course of the disease.The result showed that all patients had increased serum TSH levels at each phase in the course of the disease and the values of serum TSH in the mild group were higher than in those of the severe group. In most cases,the concentration of total serum T_4(TT_4)was significantly decreased(6.2± 3.69μg/dl)at the critical stage of the disease.The mean serum T_3 concentration patients revealed a markedly reduced trend form febrile stage to early convalescent stage,special- ly,it was the lowest in the oliguric stage.The reciprocal change in serum TT_3 and rT_3 levels was observed in hypotensive and oliguric phase. The data obtaind from this study suggested that besides a strong stress,a low serum T_3 and/or T_4 syndrome may be present during the course of the disease in most cases of EHF.The authors recommended that the dynamical analysis of serum TT_3/rT_3 may be helpful to judge the prognosis of patients with EHF.

本文对55例出血热患者甲状腺功能进行了动态观察,结果表明出血热患者血清促甲状腺素(TSH)明显高于正常人;总 T_3(TT_3)、总 T_4(TT_4)则不同程度的低于正常,反 T_3(rT_3) 与 TT_3 呈相反方向的变化,即当 TT_3 降低时 rT_3上升。上述变化以低血压、少尿期为明显,提示出血热病程中除有强烈的应激反应外,还有低 T_3及/或低 T_4综合征存在。血清 TT_3/rT_3比值的变化能反映病情的轻重。

The Structural inclusions of the upper mantle and its relicts generated by partical melting are found in the many places in the ultrabasic rocks zone in Da- labute, Tangbale and Mayila etc. in west Junggar, Xinjiang. These nodules are characteristic by their distributions in swarms. The types of rock include the spinel lherzolite, clinopyroxene-bearing peridotite, saxonite and murbruk dunite etc. The author has only studied the texture and fabric on them by meane of the universal stage. The preliminary understanding...

The Structural inclusions of the upper mantle and its relicts generated by partical melting are found in the many places in the ultrabasic rocks zone in Da- labute, Tangbale and Mayila etc. in west Junggar, Xinjiang. These nodules are characteristic by their distributions in swarms. The types of rock include the spinel lherzolite, clinopyroxene-bearing peridotite, saxonite and murbruk dunite etc. The author has only studied the texture and fabric on them by meane of the universal stage. The preliminary understanding is summarized as follows: 1. The texture of this mantle rock nodules may be divided into three types; coarse texture, porohyroclastic texture and granular crystalloblastic texture which represent the outcome of different geological structures respectiaely. They display continuous transitional series each other. 2. The fabric features of the rock marked by different texture also display definite diversity. The principal axis of the indicatrix of the forsterite gives very low gnomonic projection density in the coarse texture rocks, and no clear preferred orientation can be formed. Thereby, they indieate the chara- cteristics of weak concentration of the stress under the upper mantle environment. The principal axis of indicatrix of the forsterite gives very high gnomonic proje- ction density in the granular crystalloblastic texture rocks, its preferred orien- tation is extra clear. Therefore, it indicates a high degree centralism character- istics of the stress under the environment in the crust. The features of the gno- monic projection density of the principal axis of the indicatrix of the forsterite-ch rysolite and its preferred orientation in the porphyroclastic texture rocks lie between the above both. Evidently, the porphyroclastic texture can only be generated under the action of the strong stress. This infromation further indica- tes that the characteristics of the stress is the partial centralism under the environment in the upper mantle: 3.Based on the slip system of the main minerals and experiential data, the coarse and inset forsterite and forsterite-chrysolite can be assigned to the plastic deformation type of medium-high temperature, which was probably the product under the environment in the upper mantle. The forsterite of the gra- nular finely recrystallized and impalpable blast can be alloted to the plastic deformation type of medium-low temperature, which was probably the outcome under the environment of the earth's crust, and probably represents the outcome under the action of stress at late stage of the mantle, even at much latter stage of the mantle. Under the action of the strong stress they are not only mar- ked by mineral intergranular slip, but also intragranular slip to a varying degree. 4.Since the distribution of samples is close to the rift zone and ite gliding. plane and direction of the main minerals and key plane of the rock texture are basically in agreement with the occurrence of the rift structure, it indicates that the mode of occurrence and fabric of the nodules of the mantle rocks are contro- lled by the related depth rifts seperately, so these faults should be recognized as an ultracrust rift as for the location of occurrence, the rocks with the porphyro- clastic texture mainly came out at the nodes of many group rifts or top of the arc rift structure, while the rocks of coarse texture or granular crystalloblastic texture mainly came out at the position closing to one group rift structure or the limb of arc rift structure. In a word, all mentioned above reveals texture and fabric features of the man- tle nodules veals the evolution of mantle rocks and relationship between earth driving force and the mantle nodules. It may afford some microdata for further study of the relations among the plate structure, ophiolite and mineral resources relavent to it. Therefore, it bears certain geological and practical significance for the advance study of the texture and fabric of the mantle nodules.

本文讨论了新疆西准噶尔地区地幔岩团块的岩石类型及其结构与组构特征,并研究了不同组构特征的岩石所代表的地质环境及其与深大断裂的关系,同时还初步分析了它们的应力条件。这些研究将有助于揭示地幔岩的演化及其与地球驱动力的关系,并为进一步探讨板块构造、蛇绿岩及其与有关矿产的关系,提供一些微观数据。

The dynamic inflence not only induces deformation (including folds, faults, etc.), but also causes differentiation, migration and reconstitution of original ma- terial in rocks and ore-bed, and some compositions are concentrated in ore at different place. Four examples of iron ore deposite are described in this paper. In Daxigou, Shaanxi, the metallogenetic materials show horizontal zonation, caused by dynamic differentiation and they are ranged as protogenous siderite, transformed magnetite, chalocopyrite...

The dynamic inflence not only induces deformation (including folds, faults, etc.), but also causes differentiation, migration and reconstitution of original ma- terial in rocks and ore-bed, and some compositions are concentrated in ore at different place. Four examples of iron ore deposite are described in this paper. In Daxigou, Shaanxi, the metallogenetic materials show horizontal zonation, caused by dynamic differentiation and they are ranged as protogenous siderite, transformed magnetite, chalocopyrite and galena, located correspondingly from stronger to weker deformed area. The Wutonggou and Jianshan iron deposits, Xinjiang, occur in the same stra- ta. In Wutonggou, the ore bodies are located where the rocks had undergone medium deformation and metamorphism, accompanied with interlayer slip develo- ped between carbonatite and green schist, which enhanced the exchange of materi- al between each other, and the ores are enriched with iron by replacing Ca of the carbonatite. The Jianshan mine is located at strong deformation and metamorphic area. Owing to the loss of CO_2 and other mobile component, the original siderite ore had changed into magnetite-quartzite. The Kendekek ore district, Qinhai, is a syncline structure. It shows compo- sitional exchanges between the dolomite and volcanic rocks at the axis of sync- line where the stress was stronger than that of limb during deformation. By this way, the skarns were formed, accmopanying with the dissociating of iron from rocks to form ore. The Shilu ore district, Hainan, is a brush. structure. When the brush structure de- veloped, strong stress squeeze started at its convergent area, causing the loss of greater part of K, Na, Al, Ca and Mg and absorption of Si by dolomite, therefore iron could be concentrated to form rich ore. The fomer two examples are protogenous iron ore which had changed into rich ore by tectonic effect, and the last two are ordinary rocks which had changed into iron ore and enriched by similar way.

以青海肯德可克、新疆梧桐沟-尖山、陕西大西沟和海南石碌四个铁矿床为例,讨论了层控铁矿的动力成矿作用。原始沉积岩石或矿石所含各种组分,在动力作用下发生分异、重新组合,或在动力的压泌作用下使某些活动组分离去,从而导致原有铁质在有利的构造部位(通常是受力较强的部位)相对聚集而成矿,或使贫矿石变富。

 
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