利用阵列感应测井仪信号反演非均匀分布地层电导率

基于非线性积分方程,利用井轴上阵列感应成像测井仪（AIT）的单频测量信号,将变形玻恩（Bom）迭代方法用于地球物理测井反演,用正则化方法求出地层电导率分布。文中首先给出对于未知电导率分布的非线性积分方程,然后用玻恩近似使非线性积分方程线性化,求出电导率分布。在迭代过程中,数值模式匹配法用于求解阵列感应的正演问题。数值计算表明,用井轴上 AIT 的单频测量信号得到的成像结果与真电导率剖面分布吻合较好。     

On the relative performance of spectrum superposition methods considering modal interaction effects

The contribution of modal interaction in the various available spectrum superposition methods is accounted via the modal cross-correlation coefficient, which has been defined in several different approximate ways. Further, in these methods, to define the final expressions directly in terms of the response spectrum amplitudes, the peak factors for all the modal responses are approximated to be equal to the peak factor for the total structural response. However, these assumptions have been found to be violated significantly in many cases and do not hold good in general. Therefore, some recent studies have attempted to improve upon these assumptions. In this paper, detailed investigations are made to study the relative performance of the various available methods considering the modal interaction effects. To find out which of the available methods, in general, gives the better results, the response of a five-storey asymmetric hypothetical building, characterized by significant interaction effects, has been computed from different methods for several widely differing input excitations and the results have been compared with the exact time-history solution.     

定性地质变量分维数估计与显微地质异常

以白牛厂银多金属矿床钻孔岩心标本的高密度长序列电子探针分析数据为例,提出了定性地质时空序列变量匹配关联维数字义和分维数估计方法及分形体识别原则。     

某油田稠油油藏加密钻井工程技术

结合钻井工程实际,介绍了稠油加密钻井施工的特点,钻井设备选择、钻进工艺,泥浆工艺与完井工艺等。     

中国大陆及其周边板内地震活动的整体演化模式（一）

以活断层网络为结构框架的中国大陆及其周边地区可视为一个“断层运动与蕴震”系统。用自耦合方法初步研究发现，该蕴震系统是一个时间结构有序的耗散系统，这种时间结构的有序是在远离平衡态的条件下，通过系统与环境物质，能量的变换而建立和维持的。它在演化过程中遵循着非平衡相变的若干特点，这就是临界慢化，分岔与减熵等，以能量积累的负反馈方式开始，以能量大释放的正反馈方式结束的螺旋式地震活动周期是中国大陆及其周边板     

总磁场强度的空间相关及北黄海ML5.0级地震异常

清理攻关后，虽然相关系数法被列为地磁学科预报地震的方法之一，但应用性较差，且震例不多，为了探讨该种方法预报地震的效果，本文对辽宁地区总磁场强度进行了空间相关分析。     

Prediction method of sand-movement direction in rivers by geochemical elements

 The analysis of sand samples by X-ray fluorescent spectroscopy (XRF) gives the ratio of the geochemical elements to construct the sand samples. The application of the ratio matching to sand samples represents the correlation number between two sand samples with respect to geochemical elements. When the correlation number between two sand samples is low, the two samples are not geochemically similar each other. This denotes that the exchange of sand between two sampling points is scarce or the two samples are independent. When the correlation number between two sand samples is high, the two samples are geochemically similar, signifying that the exchange of sand between two sampling points is frequent or there is sand movement between two sampling points. If there exists prominent sand movement in the study area, the correlation number is almost 1 and kilo count number per second of each geochemical element per weight decreases along the flow direction. The decrease is caused by the reduction of sizes and the adherence of dirt on the surface of sand particles. Since the flow direction in rivers is usually the same as the direction of sand movement, it can be verified. This study obtains satisfactory results applying the method of prediction in sand movement to sediments in rivers. Received: 17 May 1995 · Accepted: 14 August 1995     

Correlation between assessments of undiscovered oil and gas resources

There is an inbuilt correlation between estimated quantities of oil and gas produced by probabilistic assessments of undiscovered oil and gas resources. Correlation between assessed quantities of oil and gas occurs at every level, whether prospects, plays, basins, continents, or the world. Providing that the oil and gas are assessed in the same run of the computer program, the correlation can be calculated using the paired values of the undiscovered oil and gas volumes calculated in each of the Monte Carlo simulations. It can be seen in the shape and density of a point plot of these paired values. Alternatively, the correlation can be calculated theoretically using an equation written in terms of the data input to the assessment program. These commonly include distributions for the number of accumulations (N), the success rate (s), the accumulation sizes (V), an oil to gas conversion factor, and a proportion of oil to oil plus gas (P _OOG). The cause of the correlation is investigated and explained using point plots and equations for a variety of input distributions. The shape and density of each plot are determined by the pattern of the numbers of oil and gas accumulations, the sizes of the accumulations, and the proportions of oil to oil plus gas. The correlation is caused by the dispersion or spread of the input distributions. It may be positive or negative, tending toward positive as the dispersions ofN, s, andV increase and the dispersion ofP _OOG decreases. The correlation indicates that there is a relationship between the undiscovered oil and gas resources that may be described by fitting a linear regression to a plot of the paired values of the total oil and gas resources. The relationship should be quoted as part of the assessment and might be used to make a better estimate of the value of the undiscovered resources.     

利用多层动态窗口影像匹配方法进行自动相对定向

介绍了一种方便实用的影像匹配方法─—多层动态窗口影像匹配法，并将其应用于自动相对定向中，得到了比较满意的结果。该匹配方法利用金字塔格网、动态窗口匹配以及最小二乘影像匹配，无需任何有关像片方位的验前知识以及物方空间的任何信息，具有很高的匹配成功率。     

新的核线相关算法——跨接法

本文研究与讨论了一种新的核线相关算法——跨接法。它是基于特征匹配的算法,即将两个“特征”连接起来构成匹配窗。由于此算法能预先消除匹配窗口之几何变形,然后再判断其灰度分布之相似性,因而它能有效地考虑由于地形起伏等原因引起的变形,提高了影象相关的可靠性。