拟合法15°波动方程有限差分串联偏移

本文把最佳拟合算法（三点和五点差分格式）及串联偏移方法应用在15°波动方程偏移中。由于拟合法的差分因子随着采样间隔、步长、速度等参数的变化而变化,因此与原有的波动方程差分偏移法相比,串联偏移方法能有效的使大倾角归位,克服频散,速度及步长可以灵活变化,运算效率高等优点。     

Conditioning of coefficient matrices of Ordinary Kriging

The solution of a set of linear equations is central to Ordinary Kriging. Computers are commonly applied because of the amount of data and work involved. There has, until recently, been little attention devoted toward the conditioning of kriging matrices. This article considers implications of conditioning upon numerical stability, instead of on robustness which has been the main focus of past work. The effect of properties of the stationary covariance matrix on the conditioning of the kriging matrix is discussed. The relationship between the covariance and autocorrelation functions allows some conclusions about the conditioning of covariance matrices, based on past work in deconvolution. The conditioning of some coefficient matrices of stationary kriging, defined in terms of either the semivariogram or the covariance, is examined.     

地震信号内插与噪音剔除（一）

信号内插与噪音剔除是相互有着有机联系的两个方面。首先讨论地震信号的内插方法,提出了一种“最佳内插算子”,从而导出了另一种“检噪算子”,它可以有效地把干扰波从记录中识别出来,并将其“剔除”出去。进而讨论空间域数据的内插问题--道内插问题。在一定的条件下,空间域数据内插与时间域内插是完全等效的,因此道内插也可以采用与时间域相同的“最佳内插算子”。地震记录上的干扰波其绝大部分表现为空间域的脉冲式干扰,所以用“检噪算子”在空间域作褶积,便能识别干扰,从而对干扰加以剔除。本文解决了一种迭代的剔除方法,取得了好的效果。     

Gravity and magnetic expression of the concealed basic and ultrabasic bodies in Chalkidhiki,Northern Greece

The anomalies which are shown on the gravity and aeromagnetic data of the Chalkidhiki peninsula of Northern Greece reveal the presence of three concealed dense and magnetized bodies. The ophiolitic belt which continues northwards of the geophysical anomalies suggests that they are caused by structures which belong to it. Multiple source Werner deconvolution shows that the lower surfaces of buried bodies in Toroneos Gulf and the one onshore are concave upwards. The northern concealed body has a width of 16 kilometers, while the southern one is 8 kilometres in width. A three-dimensional model, well constrained, gives an estimate of the dimensions of the onshore feature. The edges of the bodies, delineated by the terracing method, are formed by faults along the trend of the Hellenides orogenic belt. The edges of the body in the outer part of Toroneos Gulf may be associated with seismic swarms that occurred in the 1980s.     

改进型反褶积分层解释法——一种应用PC～1500计算机处理γ测井资料的新方法

本文吸取了现行Υ测井资料解释方法的合理部分,提出了改进型反褶积分层解释法。叙述了方法的原理及设置判别因子的原则。作者以PC-1500微机为例给出了改进后的反褶积分层解释法程序流程图。通过对模型钻孔和实际钻孔测井资料的解释,证实了方法的合理性和可行性,克服了目前平均强度法中存在的人为影响,扩大了一般分层解释法的应用范围,该法可在现场及时取得结果,提高了解释速度和质量。     

Simultaneous iterative time-domain sparse deconvolution to teleseismic receiver functions

In this paper, we present a new approach to estimate high-resolution teleseismic receiver functions using a simultaneous iterative time-domain sparse deconvolution. This technique improves the deconvolution by using reweighting strategies based on a Cauchy criterion. The resulting sparse receiver functions enhance the primary converted phases and its multiples. To test its functionality and reliability, we applied this approach to synthetic experiments and to seismic data recorded at station ABU, in Japan. Our results show Ps conversions at approximately 4.0 s after the primary P onset, which are consistent with other seismological studies in this area. We demonstrate that the sparse deconvolution is a simple, efficient technique in computing receiver functions with significantly greater resolution than conventional approaches.     

Application and verification of fuzzy algebraic operators to landslide susceptibility mapping

The aim of this study was to apply and to verify the use of fuzzy logic to landslide susceptibility mapping in the Gangneung area, Korea, using a geographic information system (GIS). For this aim, in the study, a data-derived model (frequency ratio) and a knowledge-derived model (fuzzy operator) were combined. Landslide locations were identified by changing the detection technique of KOMPSAT-1 images and checked by field studies. For landslide susceptibility mapping, maps of the topography, lineaments, soil, forest, and land cover were extracted from the spatial data sets, and the eight factors influencing landslide occurrence were obtained from the database. Using the factors and the identified landslide, the fuzzy membership values were calculated. Then fuzzy algebraic operators were applied to the fuzzy membership values for landslide susceptibility mapping. Finally, the produced map was verified by comparing with existing landslide locations for calculating prediction accuracy. Among the fuzzy operators, in the case in which the gamma operator (λ = 0.975) showed the best accuracy (84.68%) while the case in which the fuzzy or operator was applied showed the worst accuracy (66.50%).     

自动综合算子分析及算法库的建立

在分析自动综合过程和自动综合系统构成的基础上，指出了自动综合算子库对自动综合的必要性，并以现有的各种综合算子划分为参考，对自动综合算子进行了重新划分，提出了算子库中的算法集合，以此来建立自动综合算子库。