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71.
古果属(Archae fructus)研究进展及其时代的讨论   总被引:2,自引:0,他引:2  
迄今最早的被子植物—古果属(Archaefructus),包括“辽宁古果”和“中华古果”,以其对折状心皮在轴上螺旋状排列、雄蕊成对状着生、具单沟状花粉等特征。显示了它们在早期被子植物中的原始性。古果属茎枝细弱、叶子细而深裂、叶柄基部多膨突等特征。反映了该属的水生革本特征。根据对其生殖器官及营养器官等特征研究,推测该属很可能源于现已灭绝的、古老的种子蕨类。结合对其伴生的植物化石及相关地质、地理背景等综合分析,认为古果属及叉县组下部的时代为晚侏罗世,而并非早白垩世。  相似文献   
72.
This work presents a novel procedure for identifying the dynamic characteristics of a building and diagnosing whether the building has been damaged by earthquakes, using a back‐propagation neural network approach. The dynamic characteristics are directly evaluated from the weighting matrices of the neural network trained by observed acceleration responses and input base excitations. Whether the building is damaged under a large earthquake is assessed by comparing the modal parameters and responses for this large earthquake with those for a small earthquake that has not caused this building any damage. The feasibility of the approach is demonstrated through processing the dynamic responses of a five‐storey steel frame, subjected to different strengths of the Kobe earthquake, in shaking table tests. Copyright © 2002 John Wiley & Sons, Ltd.  相似文献   
73.
The Vincent Thomas Bridge in the Los Angeles metropolitan area, is a critical artery for commercial traffic flow in and out of the Los Angeles Harbor, and is at risk in the seismically active Southern California region, particularly because it straddles the Palos Verdes fault zone. A combination of linear and non‐linear system identification techniques is employed to obtain a complete reduced‐order, multi‐input–multi‐output (MIMO) dynamic model of the Vincent Thomas Bridge based on the dynamic response of the structure to the 1987 Whittier and 1994 Northridge earthquakes. Starting with the available acceleration measurements (which consists of 15 accelerometers on the bridge structure and 10 accelerometers at various locations on its base), an efficient least‐squares‐based time‐domain identification procedure is applied to the data set to develop a reduced‐order, equivalent linear, multi‐degree‐of‐freedom model. Although not the main focus of this study, the linear system identification method is also combined with a non‐parametric identification technique, to generate a reduced‐order non‐linear mathematical model suitable for use in subsequent studies to predict, with good fidelity, the total response of the bridge under arbitrary dynamic environments. Results of this study yield measurements of the equivalent linear modal properties (frequencies, mode shapes and non‐proportional damping) as well as quantitative measures of the extent and nature of non‐linear interaction forces arising from strong ground shaking. It is shown that, for the particular subset of observations used in the identification procedure, the apparent non‐linearities in the system restoring forces are quite significant, and they contribute substantially to the improved fidelity of the model. Also shown is the potential of the identification technique under discussion to detect slight changes in the structure's influence coefficients, which may be indicators of damage and degradation in the structure being monitored. Difficulties associated with accurately estimating damping for lightly damped long‐span structures from their earthquake response are discussed. The technical issues raised in this paper indicate the need for added spatial resolution in sensor instrumentation to obtain identified mathematical models of structural systems with the broadest range of validity. Copyright © 2003 John Wiley & Sons, Ltd.  相似文献   
74.
Sedimentological, cyclic-stratigraphic, paleomagnetic, and clay-mineralogical studies on the early Oligocene Yaxicuo Group in the Hoh Xil Basin, the largest Cenozoic sedimentary basin in the hinterland of the Tibetan Plateau, provide abundant information of paleoclimate changes. A 350-m thick section in the middle-lower Yaxicuo Group was analyzed to reveal the climatic history that occurred in the Hoh Xil region during the early Oligocene interval 31.30-30.35 Ma, dated with the paleomagnetic chronostratigraphy. The results indicate that add and cold climate dominated the Hoh Xil region during the early Oligocene in general, being related to the global cooling and drying events that occurred in the earliest Oligocene. Within this period, relatively warm and wet climate accompanied by strong tectonic activity occurred in the 31.05-30.75 Ma interval; while add and cold climate and relatively inactive tectonics occurred in the 31.30-31.05 and 30.75-30.35 Ma intervals. Furthermore, spectral analyses of high-temporal resolution paleoclimatic records show orbital periods including eccentricity, obliquity, and precession. It is concluded that paleoclimate changes during the early Oligocene in the Hoh Xil region were forced by both tectonic activity and orbital periods.  相似文献   
75.
路用探地雷达的应用技术研究进展   总被引:19,自引:12,他引:19  
有效、无损、快捷、简便是公路检测技术发展的方向,当前国内外先进的浅层勘探技术——路用探地雷达检测,以其无损、快捷以及浅层高分辨率的优势被迅速应用于公路检测。本文对近年来路用探地雷达技术的发展及应用情况进行了介绍,详细分析了探地雷达的工作原理、系统组成结构。就探地雷达在公路建设、维护过程中的应用情况进行了系统总结。  相似文献   
76.
TheidentificationandcriteriaofshorttermseismicitygapbeforeagreatearthquakeJINGQUANCAO(曹井泉)JIALINSUN(孙加林)YIYANG(杨毅)Seismol...  相似文献   
77.
结构参数未知条件下的地震动反演研究   总被引:29,自引:2,他引:29  
本文运用复合反演的观点研究结构参数未知条件下的地震动反演问题。根据地震作用的力学特性,将其具体化为估计输入的修正条件,文中给出了一类反演算法。理论分析及算例表明,该算法具有稳定的收敛特性以及良好的反演效果。  相似文献   
78.
吕培苓  孙士宏 《地震》1997,17(1):67-74
通过研究华北北部中强以上地震震后地震活动,地形变、地电阻率、水化学和水位变化特征,给出了各单项方法识别震后效应与新地震异常的标志。为了综合判别震后短临异常变化是震后效应或新异常,研制了一套综合识别计算机程序系统,该系统考虑了已发生的强震序列类型,地震活动背景特征以及强震前后前兆短临异常变化形态,充分利用专家的知识与经验进行推理和判断。通过运行典型事例表明该系统功能较强,使用方便。系统的实现是专家系  相似文献   
79.
A seismic re fraction/wide-angle reflection profile is analysed for the presence of correlated events ('phases'). The correlation problem is formulated in terms of temporally, spatially and frequency-local complex covariances. For robustness, the method concentrates on phase rather than amplitude information. This allows a computationally efficient algorithm that can make allowance for signal correlation length and can model curved wavefronts. A statistical test based on residual phase misfit across the analysed subarray is used to assess the probability that a detected event represents a real correlated signal.
With our chosen analysis parameters and confidence level (over 99.9 per cent). 1222 events were detected in the data. Using simple techniques based on 1-D earth models, detected events are associated with a small number of particular wave types. In this way, we have succeeded in classifying almost 95 per cent of the detected events. Those that remain describe those components of the data that are inconsistent with our simple ray paths in the 1-D assumption and with our prescribed tolerance. These include reverberations, near-surface guided waves and reflected waves from strongly laterally inhomogeneous structures. According to our modelling, about 25 per cent of the detected events are consistent with simple P -wave reflected energy, and these are to a very large extent (over 85 per cent) distinct from all the other wave-type models we have used. A direct mapping of the detected events into the offset-depth domain reveals dear internal and external consistencies among the detections for the various wave types. Estimated earth structure is consistent with models from previous analyses based on much larger data sets.
We have thus succeeded in extracting correlated events from the data and decomposing these, approximately but meaningfully, into distinct classes (ray paths)  相似文献   
80.
分离的大陆板块边缘镁铁-超镁铁岩系Th/Hf—Ta/Hf判别   总被引:1,自引:0,他引:1  
本文在论述了Th/Hf-Ta/Hf关系判别岩浆岩源区大地构造环境机理的基础上,根据世界上典型大地构造环境区岩浆岩系的Th、Ta、Hf特征,提出了分离的大陆板块边缘镁铁-超镁铁岩的Th/Hf—Ta/Hf判别标志:Th/Ta=1.8~4.0,Ta/Hf>0.1。  相似文献   
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