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Methods combined treatment with psychology, surgery and traditional chinese medicine was applied to 80 senile patients with femoral fracture by earthquake.results the incision healing of the 80 cases reached i/a; cr showed good reduction of the fracture after operation; no bedsore and deep vein thrombosis occurred; no hip and knee anchylosis and no limb muscular atrophy were found; functional restoration advanced obviously.conclusions it is effective and necessary to provide combined treatment to senile patients with femoral fracture by earthquake.

对80例高龄股骨骨折患者采用心里、手术、中药、跨学科的康复综合治疗对治疗结果进行分析,总结经验。结果 80例患者手术后切口ⅰ/甲,cr片骨折对位对线好,无褥疮及下肢深静脉血栓形成,髋膝关节无僵硬、肢体肌肉无萎缩,功能康复明显提前。结论对地震伤高龄股骨骨折患者采取心里、手术、中药、跨学科的康复综合治疗是必须的,可行的。地震伤;高龄骨折;治疗

Many of the men and women who live at Two Kings view the earthquake as a comeuppance for man's endless wars, the neglect of the elderly, the abuse of the environment.

住在寺庙的许多人认为地震是对人类无止境的战争,是对长者的不孝顺,是对人类破坏环境的惩罚。

From 2004 to 2007, small horizontal different movement (1.6 mm/a), especially dextral movement, shows in the middle piece of Longman Mountain.

结果表明,发生汶川8.0级地震的龙门山断裂带1999~2004年相对稳定的华南地块无明显的相对运动,2004~2007年有一定程度的相对运动显示,以右旋活动为主,年速率为1.6mm/a。

By means of different subjects and te chniques,the paper makes an overall study on the crustal stability of Beihuaiyang region and its adjace nt areas from the aspects of current t ectonic stress fields,principal fa ult structures,analysis of regional fa ults and neotectonic activity,seis mic activity and numerical modeling,etc.

运用多学科、多技术相结合的研究方法,从现今构造应力场特征、现代地壳形变特征、主干断裂构造以及区域断裂活动性分析、新构造运动、地震活动、数值模拟等方面入手,对北淮阳及其邻接区地壳稳定性进行了全面而系统的研究,指出本区地震活动受走滑活动断裂控制,中、强地震集中于区内东南部和西北部NW向与NE向断裂交汇处;第四纪无大规模差异升降运动;数值模拟等综合分析表明,信阳地区的区域构造稳定性高,现代地壳形变量小,应力平缓,地震活动少且弱。

There, they find that the anomalous groups are variety,similarity and periodicity of development before and after Baotou Ms 6. 4 earthquake, this is similar to Haicheng and Tangshan earthquakes, however, the obviously difference is that the abnormal is no causality and associated relation but paragenic relation with Baotou earthquake. They think the circum --B...

该区异常群体具有种类的多样性、配套性,在包头6.4级地震前后有发展阶段性,虽与海城、唐山地震前确有相似之处,但也有明显不同,认为环渤海地区参与了1996年以包头地震为代表的华北整体性构造活动,该区异常与包头地震无因果或伴生关系,而是共生关系,该区目前仍存在发生5~6级或6级以上地震的危险性。

In viewpoint of the lack of enough basic data of foreign oilfields, under the conditions of insufficient core data, no constrains of seismic interpreted cross and fault data, the rational fine 3D geological model has been established by fine oil reservoir characterizing technique including the contrast results of individual layers, second well logging interpretation and so on.

针对国外油田多数基础资料不全,必须在缺乏取心资料,无地震解释层面及断层数据约束的条件下,运用层序地层学小层对比结果和二次测井解释等精细油藏描述技术,并插入虚拟井控制井间构造,进而建立了合理的精细三维地质模型,为该油田的储层预测及数值模拟提供了基础数据,并在实际应用中取得了良好效果。

The main methods we adopted including infrasonic wave, crustal stress, geoelectricity, micro vibration of the earth and tide generation of force resonance, etc.

我们经过 2 0多年的临震前兆观测研究发现:目前我们所了解的地震前兆观测方法都存在非震异常现象(即有前兆异常,并无地震发生)。

No forefront of the history of the 8 earthquake, but also to the Chinese earth tremors followed.

这场史无前列的8级地震,也让华夏大地随之震颤。

Characteristics and principles of time clustering and frequency with a seismic sequence of more 380 years (1615 —1998) are performed using fractal theory and rescaling range analysis theory. It is concluded that the fiactal dimensions of seismic subset are similar to each other, the mean value is about 0.405, and interval of scale invariance can change 1-2 magnitude order. It is also found that the Hurst index ranges from 0.5412 to 0.5580. The results show that there is of statistical self-similar among different magnitude earthquakes in the area of bridge site.

应用分形理论和R/S分析原理,编写了程序,分析和研究了桥址区的380多年(1615~1998)地震序列的地震时间从集和地震频度特征及规律,得出桥址区不同震级范围的子集合具有近似相等的分维值,约为0.405,子集合无标度区可跨1~2数量级;不同震级层次的地震频度Hurst指数为0.5412~0.5580,都表明了桥址区不同震级层次的地震之间具有统计自相似性。

The Xujiahe formation in south Sichuan basin is featured by continental clastic sedimentary, thin sand mud interbed, and the welldeveloped sandstone in this area, however, its lithology is tight and its physical properties is poor. In the case of gas bearing, the acoustic velocity difference between the sandstone and the shale is too little to make clear responses on seismic data, as a result, it is very difficult to conduct the gasbearing prediction and to analyze the gasbearing range distribution by means of conventional impedance inversion and hydrocarbon detection.

四川盆地蜀南地区上三叠统须家河组为一套砂泥岩互层的陆相碎屑岩沉积,砂岩发育,但岩性致密,物性较差,砂岩储层含气后的速度与页岩速度相差不大,在地震剖面上无明显的响应,因而采用常规波阻抗反演和含气检测技术不能有效解决该类含气储层识别问题和含气范围展布问题。

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