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characteristics of activity
相关语句
  活动特征
     CHARACTERISTICS OF ACTIVITY OF RECENT VERTICAL DEFORMATION FIELD AND PRELIMINARY EXPLORATION ON ITS RELATION TO FUTURE EARTHQUAKES IN SHANDONG PROVINCE
     山东近期垂直形变场活动特征与其未来地震的初步探讨
短句来源
     RECENT CRUSTAL VERTICAL MOVEMENT IN JIANGSU-SHANDONG-ANHUI AREA AND CHARACTERISTICS OF ACTIVITY IN TANCHENG-LUJIANG FAULT ZONE
     苏鲁皖地区现今地壳垂直运动及郯庐断裂带的活动特征
短句来源
  “characteristics of activity”译为未确定词的双语例句
     PRELIMINARY ANALYSIS OF CHARACTERISTICS OF ACTIVITY PATTERNS OF M≥6 EARTHQUAKES IN SOUTHWESTERN CHINA AND ITS ADJACENT AREAS
     我国西南及其邻区M≥6级地震活动图象特征的初步分析
短句来源
     The experimental results prove that its main technical indications have greatly exceeded those of Type ICI 741 catalyst, and it has the remarkable characteristics of activity at low temperature, high catalytic activity, heat tolerance, resistance to poisoning, and high mechanical strength.
     实验结果证明,ZA5型氨合成催化剂的主要技术指标已大大超过ICI741型氨合成催化剂,具有活性温度低、催化活性高、耐热和抗毒性能好及机械强度高等显著特点
短句来源
     Characteristics of activity and sediment of wind-sand current in Xinjiang line of New Eurasian Continental Bridge
     新亚欧大陆桥新疆段风沙流活动特性及停积规律
短句来源
     Study on characteristics of activity oxygen and plasma permeability in leaves of different types tall fescue varieties in different temperature stress
     温度胁迫下外引高羊茅活性氧代谢与细胞膜透性的变化
短句来源
     and then we randomly select 61 3-to-5-year-old children and observe their characteristics of activity in the laboratory.
     在以上研究的基础上,随机选取61 名3~5 岁儿童对其活动性进行实验室观察,并由其父母填写《父母教养方式问卷》。
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  相似匹配句对
     And the characteristics of the G.
     通过仿真和实验,也验证了G.
短句来源
     characteristics;
     三、发展的特点;
短句来源
     On the Intrinsic Characteristics of Leading Activity
     论领导活动的本质特征
短句来源
     The characteristics of G.
     论文首先对语音编码的各种方案进行了比较,并对G.
短句来源
     Basic characteristics of Secretary Activity
     对秘书活动基本特征的探索
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  characteristics of activity
Comparative characteristics of activity in grafted and intact neocortex in slice preparations
      
The difference in the characteristics of activity is connected with the geometry of the dendrites and the foci of their maximal branching.
      
Changes in phase characteristics of activity of the vascular system revealed by rheography in dogs at different age periods
      
Characteristics of activity energetics of the UV cet-type flare stars
      
The capacity of the pedometer to detect the impacts of body movements, and the characteristics of activity, are responsible for the differences in correlation.
      


By analytic calculation of the Weibull distribution,we obtain a parameter E(T) which is dependent with the probable distribution function of strong earthquake occurrence,then applying this parameter.We analyse quantitatively these strong earthquakes (B.C.780-11,1976;M≥6) at the crust and upper mantle in China.First,we use materials of solutions for earthquake mechanism and analysis of stress fields to regionalize different zones of strong earthquake in China based on different characters of stress fields,and...

By analytic calculation of the Weibull distribution,we obtain a parameter E(T) which is dependent with the probable distribution function of strong earthquake occurrence,then applying this parameter.We analyse quantitatively these strong earthquakes (B.C.780-11,1976;M≥6) at the crust and upper mantle in China.First,we use materials of solutions for earthquake mechanism and analysis of stress fields to regionalize different zones of strong earthquake in China based on different characters of stress fields,and then with the Weibull distribution theory,We obain the E(T) of different earthquake zones,thus one characteristic of activity in China's strong earthquakes is given,i.e.the characteristic of time interval for the recurrence of strong earthquake,and from that to obtain the probable distribution of strong earthquake ocurrencc in every earthquake zone.Among them,earthquakes with M≥7 the E(T) are 208 years for north China,177 years for the north-west zone,80.5 years for Sichuan-Yannan zone,37 years for Xinjiang zone,10 years for Taiwan zone and 9.8 years for Xizang zone.The difference of E(T) and probable distribution between every zone reflect different characters of the activity for in-plate strong earthquakes and plate border strong earthquakes,and also reflects different characters possessed by strong earthquakes of the different zones in plate.The existence of these different characteristics spontaneously reflects that the different influence exerted by the India Plate,Pacific Plate and Philipine Plate on China Continent leads to a synthetic result.

本文导出与地震活动有关的两个参数m和E[T]以及地震发生的概率分布函数,并由中国大地震资料求出中国各地震区的这两个参数值和大地震发生的概率分布。其结果是:(1)中国各地震区的判断性参数或地震发生方式参数m值均大于-1,证明中国大地震具有一个共同特征——其发生方式为周期性的;(2)中国各地震区的地震活动性参数或同一地点范围内大地震复发的优势时间间隔E[T]值随震级而异,随地区而异。即震级越大其值也大,反之亦然。板缘地区其值较小,板内地区其值较大,离板缘越远其值越大;(3)中国各地震区大地震发生的概率分布曲线也与震级和地区有关。即震级越大,曲线越缓,震级越小曲线越陡。板缘地区曲线较陡,板内地区曲线较缓,且离板缘越远曲线越缓。m、E[T]和地震发生的概率分布函数不仅对研究大地震及共预报是有一定意义的,而且对研究中小地震活动也是适用的。

Based on multi-period data of vertical deformation and geological tectonic background in Jiangsu-Shandong-Anhui area from 1953 to 1995,the features of recent crust movement in the area and the activity in Tancheng-Lujiang fault zone are studied. The conclusions are as follows:(1)The Tancheng-Lujiang fanlt zone across the studied area controls the tectonic activity in the area.(2)The activity feature of the fault zone is tensile and compressive in turn. When the fault zone is under compressive...

Based on multi-period data of vertical deformation and geological tectonic background in Jiangsu-Shandong-Anhui area from 1953 to 1995,the features of recent crust movement in the area and the activity in Tancheng-Lujiang fault zone are studied. The conclusions are as follows:(1)The Tancheng-Lujiang fanlt zone across the studied area controls the tectonic activity in the area.(2)The activity feature of the fault zone is tensile and compressive in turn. When the fault zone is under compressive movement, the ground uplifts along the fault zone as the direction of main pressure stress is in NNE direction, and when under tensile movement, the ground subsides along the fault zone as the direction of main tensile stress is in NE direction.(3)The new compressive movement began at about 1993 and is strengthening now. (4)The characteristic of activity in the fault zone shows left-lateral slip in the recent period.(5)The main stress direction of compressive or tensile movement is not the same(the difference between them is about 45°).

根据苏鲁皖地区1953~1995年多期精密复测水准资料,以及地质地貌构造背景,研究了苏鲁皖地区的地壳垂直运动及郯庐断裂中南段现今的活动特征,获得如下结论:(1)横穿本区的郯庐断裂带的活动直接控制着本区的构造活动;(2)郯庐断裂的活动特征为张压交替;(3)约自1953年开始,苏鲁皖地区地壳运动的演化顺序为张→压→张→压;新的“压”性运动约始于1993年,目前正在加强;(4)郯庐断裂带近期运动性质为左旋走滑;(5)张、压运动并不处于同一方向上(彼此相差约45°)。

A study is made of the activity and kinetics of Type ZA5 ammonia synthesis catalyst. The experimental results prove that its main technical indications have greatly exceeded those of Type ICI 741 catalyst, and it has the remarkable characteristics of activity at low temperature, high catalytic activity, heat tolerance, resistance to poisoning, and high mechanical strength.

对ZA5型氨合成催化剂的活性及动力学进行了研究。实验结果证明,ZA5型氨合成催化剂的主要技术指标已大大超过ICI741型氨合成催化剂,具有活性温度低、催化活性高、耐热和抗毒性能好及机械强度高等显著特点

 
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