隔震建筑结构的强震观测与初步分析

福建省防灾减灾隔震大楼自2005年8月架设强震观测结构台阵以来,已多次记录到大楼地震动力反应,这些宝贵的结构反应资料对于评价隔震效果、分析结构反应特性具有十分重要的价值。本文从中选取了震级在3.7~7.6、震中距在189~3 595km的24次地震的台阵资料,对大楼的振动特性和隔震效果进行了初步分析,得到的结论是:(1)大楼场地土层的特征周期在0.63~0.68 s;(2)中心大楼在小地震作用下表现的振动卓越频率分别为4.7Hz(垂直向)、1.31Hz(南北向)、1.40Hz(东西向),大楼水平向第一阶振型的频率分别为1.41Hz(南北向)、1.59Hz(东西向),即自振周期为0.70 s(南北向)、0.63 s(东西向);(3)大楼在小地震时隔震效果不明显,其南北向隔震效果比东西向好;随着地下室记录峰值的增大,顶层放大倍数有所降低,大楼卓越频率也有所降低;(4)初步分析表明大楼在小震时仍有扭转效应,其扭转周期为0.5 s,有待进一步分析。     

Joint probability density function of the stochastic responses of nonlinear structures

The joint probability density fimction （PDF） of different structural responses is a very important topic in the stochastic response analysis of nonlinear structures. In this paper, the probability density evolution method, which is successfully developed to capture the instantaneous PDF of an arbitrary single response of interest, is extended to evaluate the joint PDF of any two responses. A two-dimensional partial differential equation in terms of the joint PDF is established. The strategy of selecting representative points via the number theoretical method and sieved by a hyper-ellipsoid is outlined. A two-dimensional difference scheme is developed. The free vibration of an SDOF system is examined to verify the proposed method, and a flame structure exhibiting hysteresis subjected to stochastic ground motion is investigated. It is pointed out that the correlation of different responses results from the fact that randomness of different responses comes from the same set of basic random parameters involved. In other words, the essence of the probabilistic correlation is a physical correlation.     

天津静海-津南剖面地壳上地幔电性结构特征

在天津市区南部的静海-津南一线布置了32个大地电磁测深点,剖面方位角92°,对采集的资料采用远参考与Robust技术进行了处理和解释.对该区的构造维数及构造方向做了分析,揭示了该剖面地壳上地幔电性结构特征,并进行了划分.成果显示:中下地壳存在双层低阻构造层,上地幔表现为中、高阻互层.在断裂带附近受构造活动影响,低阻高导构造层会发生上下错断与缺失.沧东、白塘口、天津断裂均是多组断层构成的断裂带,控制了双窑凸起、白塘口凹陷、板桥凹陷及静海斜坡带次级构造单元.     

距离平方反比法矿产资源储量计算模块设计与实现

固体矿产储量计算的传统方法,如地质块段法、断面法等计算结果精度底,计算过程繁琐,不方便利用计算机技术.经典的地质统计学储量计算方法日趋成熟,便于充分利用计算机软件技术,计算速度快,精度高.文章讨论了距离平方反比法储量计算模块的设计过程、模块功能的实现方法、过程和结果,重点分析了如何利用给定品位提取范围动态地计算矿体储量、结果可视化及计算结果精度的检验方法.最后评价了该方法的优缺点.用距离平方反比法计算矿体储量,不仅可以提高计算结果的精度,降低计算方法对矿体形态和控矿工程的依赖程度,而且能够通过矿体品位模型确定矿体在三维空间的展布状况,实现了计算结果的三维可视化.     

冰川下垫面对夏季云结构和云水含量的影响——以祁连山区疏勒南山为例

云水含量和云结构参量是天气预报、高山区水循环过程分析的基础.基于2012—2015年夏季CloudSat卫星遥感资料的2B-CLDCLASS、2B-GEOPROF和2B-GEOPROF-LIDAR,结合中国第二次冰川编目数据及气象资料,对祁连山地区疏勒南山冰川区与非冰川区云水含量和云类型特征进行分析.结果 表明:(1)...     

金沙江白鹤滩水电站坝址区断层变形特点及成因分析

拟建中的白鹤滩水电站坝基将建在二叠系峨眉山组玄武岩层之上.坝址区发育有位移量较小的NW300°、NW320°、NE40°和近SN向4组断层,其中NW300°断层最为发育.在野外详细调查的基础上,室内的显微构造研究和电子自旋共振(简称ESR)测年结果表明,坝址区内的断层是在燕山期晚期近东西向挤压应力场作用下形成,后期又受到了近南北向挤压应力场的改造.断层破碎带以发育典型碎裂-角砾岩等浅层脆性构造岩为特点,近期活动不明显.     

基于速度场模型的区域CGCS2000坐标实时转换

从WGS84到CGCS2000的坐标转换,涉及坐标框架转换和历元转换两个问题.如何提高大区域坐标转换精度,是一直以来的研究热点,针对大区域坐标转换精度较低的问题,考虑历元转换,提出融合速度场改正信息的坐标转换方法.该方法对建立速度场改正模型进行了研究,分析比较了各模型的精度和可靠性,在此基础上选择一种模型用于实现CGC...     

折射层析成像法测试隧道围岩松动圈

通过应用折射层析成像法在乌鞘岭特长隧道中的测试,说明该方法对于横向速度变化不均一,过渡带速度渐变的地质情况具有分辨率高、图像直观、易于解释,适合对隧道围岩松动圈的测试.     

Structure Refinement of Cs-rich Na-Li Beryl and Analysis of Its Typomorphic Characteristics of Configurations

1 Introduction Natural beryl is an accessory mineral mainly in pegmatite, partly in some highly diffractionated granite or metamorphic rocks, with the crystal shapes beingprismatic, or occasionally tabular. For tabular beryl found in pegmatite it is believed that the tabular configuration is connected with alkali metals (Bieus, 1960; Wang et al., 1981) and geneses of the tabular configuration have been reported before. In recent years, tabular beryl has been found in the Xuebaoding W-Sn-Be d…     

Provenance of Precambrian Fe- and Al-rich Metapelites in the Yenisey Ridge and Kuznetsk Alatau, Siberia： Geochemical Signatures

Major, trace and rare earth element contents of Fe- and Al-rich metapelites from the Korda （Yenisey Ridge） and Amar （Kuznetsk Alatau） formations were determined to examine the nature, origin and evolution of their protoliths. Results indicate that these rocks are the redeposited and metamorphosed products of Precambrian kaolinitic weathering crusts, while the geochemical distinctions between the studied metapelites are determined by different weathering conditions in the source area and tectonic settings. The protolith of the Korda Formation metapelites was produced by erosion products of the post-Archean granitoid rocks, which accumulated under humid climate conditions in shallow-water basins along the continental margin. The geochemical characteristics of the deeper primary deposits of the Amar Formation suggest that volcanogenic material of mafic composition derived from an island-arc environment had a major role in supplying the erosion zone. These results agree with lithofacies data and with the geodynamic reconstruction of the evolution of the Yenisey Ridge and Kuznetsk Alatau during the Mesoproterozoic and Neoproterozoic, respectively. It was shown that REEs had limited mobility during contact metamorphism. The coherent mobility of REEs during collisional metamorphism may be attributed both to mineral reactions responsible for modal changes and to local chemical heterogeneity inherited from the initial protolith.