The Analysis of Three Dimensional FEM for Interaction of the Gravity-arch Dam and Complex Ground at Geheyan,Qingjiang River

This paper introduces the analysis of three dimensional finite element method for the gravity-arch dam building on the complex ground. The foundation rock of dip and strain-slip, three faults, two weak intercalations and etc. arc considered in this calculation model. Water static pressure, gravity of dam, uplift, temperature stress and so on are computed, including three dimensional osmotic and temperature fields in the foundation. The range of calculation model is about 1400×900×600m2 . There are 1845 elements of all kinds, 3280 nodes in the network of finite element. The superlax iterative method is used to solve, and three dimensional perspective and software of after treatment are applied in analyses. The dimension of this computation is large, various results of treating complex problems are reasonable. The important basis has applied to designing unit. The computation is important practical significance for Geheyan Dam which is being built.     

新疆特克斯-昭苏地震断层的发现及有关问题的讨论

1986年作者在特克斯-昭苏盆地首次发现长70公里、最大垂直和水平位移均达8米的地震断裂带和地震形变现象,并认为是1716年地震时形成的。地震断裂带的展布和运动方式,与科博河-昭管处断裂相一致。特克斯断裂带是一条复杂的断裂带,它由多条断裂组成。1716年地震表明该断裂带具有新的活动性     

华南地区中生代以来构造应力场的基本特征

本文认为,华南地区于燕山旋回中早期主压应力轴是北西——南东和北西西——南东东向的。燕山晚期以来,主压应力轴基本上是北东——南西和北东东——南西西乃至近东西向的。     

系统聚类法在华北地区的地震分期和预测中的应用

本文用修改了的系统聚类法研究华北地区地震活动期,结果表明,当类间距离用离差平方和增量距离,且样品间用欧氏距离时,能较好地划分该地区的地震活动期。而样品间用相似系数时,不论类间距离是哪一种,所得结果均较差。本文还作了地震活动期的后验预测尝试,还通过逐次筛选方法对21个特征进行了选择。     

IMAGE PREDICTION FOR TORRENTIAL RAIN AREAS

A new method is presented for the prediction of a torrential rain (TR) area, where some atmo-physical parameters are used with their given values as criteria most favorable for the occurrence ofTR; an over-all examination is done of the relative favorabilities of these factors for the TR productionin other regions which are then composited and numeralized by means of the theory of nonlinearmapping with the results plotted (‘reflected') on a weather chart, allowing to make an objectiveforecast of the TR area. The preliminary results indicate that the technique is able to objectivelycomposite and clearly exhibit principal distribution features of the parameters on the map, thus show-ing a certain amount of effectiveness for the diagnosis and prediction of a TR area. Regression analysis is used for factor selection to automatically discriminate and locate the jet-stream axis with the aid of a computer. In the calculation of the mapping the gradient method isadopted, in the light of the functional properties of the optimized index K, in place of the simplerelaxational iteration now in general use, thus getting rid of the non-convergence by the iterationmethod because of the increased number of the samples used. The square of the gradient mod-ulus <10~(-4) is set to be the criterion for the iteration convergence. The improved method canmeet the requirements of operational forecasts generally with 50 or less iterations.     

华北石炭系清水、浑水沉积交互的模式初探

地史时期中,清水与浑水沉积交互的现象非常普遍。这一沉积特征已引起了煤沉积学工作者的兴趣。华北石炭纪含煤岩系中的碳酸盐清水沉积常常受到陆源物质的强烈干扰,碳酸盐台地的存在与海水进退,古陆的“活跃”程度及沉积区、物源区的地形地貌等因素密切相关。在以上因素的综合作用下,台地或被陆源碎屑完全占据而消亡,或与之共存,在横向上犬牙交错形成了华北中晚石炭世陆表海清水、浑水沉积交互共存的复杂古地理景观。     

特征分析模型构造原理

本文研究在矿产资源评价中适用于不同条件的,特征分析模型的构造原则和方法:建立一般特征分析模型的最大标度准则;变量权和样品关联度的不同算法和解释;基于不同相似性度量标准的矿床模型及建立广义矿化模型的方法;构造多维特征分析模型和进行定量资源评价的可能性。     

漳州地热普查区地球化学异常的讨论

本文以漳州热田为例,通过对该区的地质及构造特征、地下热水分布、水化学特征及土壤地球化学异常的分析对照,论证了化探工作在地热勘查中的应用效果。同时,对热田的化探异常成因进行了初浅的探讨。     

东秦岭寒武纪构造古地理概况

本文提出寒武纪以商丹断裂带为界,东秦岭地区北部属中朝板块南部陆缘区,为主动大陆边缘,以双列岛弧为特征;中部和南部属杨子板块北部陆缘区,由两隆(大陆区北缘和中秦岭微板块)—凹(南秦岭盆地)组成,为被动大陆边缘。     

中国石炭纪古生物地理与古气候

本文从分析沉积及生物群出发,结合世界构造古地理和气候分带,将中国早石炭古生物地理分属三个生物区,即华夏生物区,中蒙海生物区和东冈瓦纳生物区。晚石炭世的生物分区与早石炭世大体相似。中国早石炭世的古气候分为华夏热带—亚热带区,准噶尔—兴安北温带区和西藏南部南温带区。其界线大致与古生物地理分区相合。晚石炭世中国气候分带与早石炭世相似。