Statistical moment-based structural damage detection method in time domain

A novel structural damage detection method with a new damage index,i.e.,the statistical moment-based damage detection(SMBDD) method in the frequency domain,has been recently proposed.The aim of this study is to extend the SMBDD method in the frequency domain to the time domain for building structures subjected to non-Gaussian and non-stationary excitations.The applicability and effectiveness of the SMBDD method in the time domainis verified both numerically and experimentally.Shear buildings with various damage scenarios are first numerically investigated in the time domain taking into account the effect of measurement noise.The applicability of the proposed method in the time domain to building structures subjected to non-Gaussian and non-stationary excitations is then experimentally investigated through a series of shaking table tests,in which two three-story shear building models with four damage scenarios aretested.The identified damage locations and severities are then compared with the preset values.The comparative results are found to be satisfactory,and the SMBDD method is shown to be feasible and effective for building structures subjected to non-Gaussian and non-stationary excitations.     

阿萨巴斯卡盆地铀矿省(加拿大):基底和其他区域构造

阿萨巴斯卡盆地的铀矿床与其他省的不整合型铀矿床不同,其主要特征是:Ⅰ)具有非常高品位铀矿石(大约是别处相似矿床品位的10倍),Ⅱ)富多金属的Ni、As、Co等矿化,Ⅲ)多数矿床是产于盖层内(在不整合中和直接产于不整合上)。尽管阿萨巴斯卡盆地的矿床特征都有些变化,但其大多数矿床的共同特点,是它们在空间上与下伏基底的早元古代黑色页岩共生,这种页岩在阿萨巴斯卡盆地沉积之前大约19—18亿年的哈德森造山运动期间发生了陡褶皱和变质(石墨化)。但是,上(阿萨巴斯卡)砂岩不整合     

根据费尔干纳预报实验场的研究结果分析治尔加塔尔地震的水文地质地震前兆

1984年10月26日22点22分19秒(格林威治时间)在治尔加塔尔(南天山)发生了5.9级地震。乌兹别克斯坦境内的费尔干纳实验场位于最活动的地震带,实验场的综合预报台网离这次地震的震中最近。 该台网综合观测了水文地质地震参数和形变测量参数、地球物理场和可以作为地震前兆的其它指标的变化。 多年的研究结果表明,在天山造山带M≥5的壳下地震和帕米尔—兴都库什M≥6的深源地震之前,都发生了水文地球化学异常和流体地球动力学异常。 流体地球动力学前兆:在奇米昂构造区利用Ⅺ、ⅩⅤ和OⅡ-Ⅰ号井观测了动态,这三口     

具有经济性前景的粗岩屑堆天然冷能集聚分析

The coarse-detrital deposits have the properties of cold accumulation and maintenance of cold for a long time. Now, at some place where the mean annual temperature of air is positive, one even can get the permafrost by artificial formation of the burial mound. According to these properties, some lowenergy storehouses are built for various purposes.     

大陸漂流过吗?

自从伊丽莎白一世女王的医生威廉·吉尔勃特以来,人们就已经知道了在地球的中心,好像有一个巨大的磁铁在起着作用。正是由于这个中心磁铁发挥了磁力,才使罗盤磁针指向接近于地理北方,才使航海员能够利用罗盤来指导航行。     

关于科拉片岩带含金条带状铁建造的说明

引言地盾区太古宙绿岩带中某些条带状铁建造的含金特征,已广为人知。科拉尔片岩带是南印度地盾的“古老绿岩带”,含有大量的条带状铁建造。条带状铁建造岩层广布于科拉尔片岩带内,在成分上是均一的。另方面,沿片岩带西边缘产出的条带状铁建造层,在走向上很稳定,延伸数公里。条带状铁建造层是以硫化物相为特征的。早期地质工作者已指出这些硫化物相铁建造的含金特征。本文的目的是介绍科拉尔片岩带不同部     

在中国几个地区进行的大地电流法勘探工作

在中国,自从1957年起,与各种地球物理方法（解决石油地貭任务）广泛发展的同时,比較年輕的大地电流法也得到了很大的发展。大地中存在大地电流,这在一百多年前就知道了。以往的观測表明,大地电流具有脉动性貭,它的大小和方向随时間而变化,并在地球表面很多地区同时出現。大地电流的产生、它的变化以及与地磁場的关系,还沒有搞得相当清楚,这是一个需要进一步研究的問題。     

中国与美国矿产资源类比及预测

作者运用单位区域产值矿产评价方法,估计了中华人民共和国的矿物和能源资源.资源估计主要立足于中国与美国50个州的地质比较.估计结果表明,中华人民共和国主要金属矿产和能源资源蕴藏丰富.     

海岸带泥砂运动的形态学与岩石学的研究方法

在苏联,近十年来,海岸地貌学的研究有了很大的发展,而对于海岸地带,即海与陆相互作用地带的泥砂运动及其迁移规律性的研究则是其中最重要的一个方向。实际上,正像所指出的,对岩石圈物质迁移过程的研究是从“岩石颗粒及原生岩塊的破碎开始直到它们在地质作用中重新结合为止”而且是作为研究地壳表面地形的形成及共发展的地貌学中的一个重要任务。正是在这个作用的过程中及其后果,就建立着并发展着各种地形的形态。通常,这些形态可划分为二种基本类型:剥蚀的和堆积的。     

Constraints of Mantle and Crustal Sources Interaction during Orogenesis of Pre- and Post-collision Granitoids from the Northern Arabian-Nubian Shield: A Case Study from Wadi El-Akhder Granitoids,Southern Sinai,Egypt

The Egyptian older and younger granitic rocks emplaced during pre- and post-collision stages of Neoproterozoic Pan-African orogeny, respectively, are widely distributed in the southern Sinai Peninsula, constituting 70% of the basement outcrops. The Wadi El-Akhder, southwestern Sinai, is a mountainous terrain exposing two granitoid suites, namely the Wadi El-Akhder Older Granites (AOG) and the Homra Younger Granites (HYG). The AOG (granodiorites with subordinate tonalite compositions) have geochemical characteristics of medium-K calc-alkaline, metaluminous to mildly peraluminous granitoids formed in an island-arc environment, which are conformable with well-known Egyptian older granitoids rocks, whereas the HYG display calc-alkaline to slightly alkaline nature, peraluminous syeno-, monzogranites and alkali feldspar granites matching well those of the Egyptian younger granites. With respect to the AOG granitoids, the HYG granites contain lower Al2O3, FeO*, MgO, MnO, CaO, TiO2, Sr, Ba, and V, but higher Na2O, K2O, Nb, Zr, Th, and Rb. The AOG are generally characterized by enrichment in LILE and LREE and depletion in HFSE relative to N-MORB values (e.g., negative Nb and Ta anomalies). The geochemical features of the AOG follow assimilation-fractional crystallization (AFC) trends indicative of extensive crustal contamination of magma derived from a mantle source. The chemical characteristics of the AOG are remarkably similar to those of subduction-related granitoids from the Arabian-Nubian Shield (ANS). The compositional variations from monzogranites through syenogranites to alkali feldspar granite within HYG could not be explained by fractional crystallization solely. Correlating the whole-rock composition of the HYG to melts generated by experimental dehydration melting of meta-sedimentary and magmatic rocks reveals that they appear to be derived by extended melting of psammitic and pelitic metasediments, which is similar to the most of younger granitic suites in the ANS.