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基于ArcGIS的西安市地震小区划数据管理系统 总被引:1,自引:0,他引:1
建立基于GIS平台的数据管理系统是陕西省防震减灾“十一五”重点项目西安市地震小区划项目中的一项重要工作,通过对该项目多源成果数据的分析,确定以ArcGIS软件为开发平台,建立地震小区划数据管理系统.提出了实现该系统须具备的基本功能、系统的基本框架,并对概念模型设计、逻辑模型设计、物理模型设计等关键环节进行了数据库详细设计.最后,对入库数据的数据准备、数据生成、数据入库等技术环节做了详细论述,这些工作将有助于实现西安市地震小区划成果数据的有效组织与管理. 相似文献
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本文在现有前兆数据观测采集传输、存储的基础上,开发研制了前兆数据差错管理系统。该系统基于Windows平台上采用Access数据库,用ADO作为连接数据对象,使用Visual Basic6.0开发工具与数据库技术相结合,实现了数据文件检查、观测日志检查、差错情况管理等多种功能。保证了数据文件的连续、完整和准确,科学有效地对数据进行质量控制。 相似文献
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本文研究地震映像数据的时频解释方法.采用短时傅立叶变换方法获得地震映像记录频谱的时间与空间分布,根据介质对地震波频谱影响的基本规律,通过分析已知地质断面地震映像记录频谱的时间与空间分布,研究了综合利用频率域和时间域信息进行地震映像数据解释的效果.时频分析方法提取了地震波的频谱中关于地层岩性、构造方面的信息,为地震映像数据的处理和解释提供了更多的参考信息.实例证明,利用时频分析解释地震映像数据,有助于了解覆盖层下岩性变化、薄层的分布范围、探测隐伏土洞、确定混凝土构件中缺陷位置,提高地震映像数据的解释精度和准确性. 相似文献
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微山湖湖区表层地震地质条件十分复杂,芦苇丛生,三维地震勘探野外数据采集采用自行研制的钻井平台加套管护壁的成孔工艺,沼泽检波器加上加长尾椎,提高了检波器的耦合效果,获取了高信噪比的三维地震数据。资料解释应用了三维可视化、相干数据体、地震属性技术进行三维构造精细化解释,明显提高了地震解释识别地下小地质构造及地震异常体的能力,它完善和发展了三维高分辨率地震勘探技术,扩大了地震勘探的应用范围,为解决煤矿开采阶段所遇到的构造、煤层等地质问题提供了一种综合应用的解释方法,在湖区的勘探开发中,取得了明显的地震地质效果。 相似文献
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对不同的小波变换算法和小波基函数进行了研究,得到了适用于地震资料处理的最佳小波基函数,并用Visual C 语言开发了基于Windows操作平台下的地震资料小波剖面制作系统。利用小波剖面制作系统和最佳小波基函数对煤田实际地震资料进行了处理,取得了令人满意的地质效果。 相似文献
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Sławomir Jerzy Gibowicz 《Acta Geophysica》2006,54(2):142-157
The following criteria for selection of doublets at Polish coal mines were accepted: the difference in magnitude (based on
seismic moment) of two events not larger than 0.15, the distance between their hypocenters not greater than 150 m, and the
time interval between their occurrence not longer than 10 days. Similarly, the criteria for seismic events at copper mines
are: the difference in magnitude not exceeding 0.15, the distance not greater than 200 m, and the time interval not longer
than 20 days. Seismic events from the Wujek and Ziemowit coal mines that occurred between 1993 and 1995, and seismic events
from the Polkowice copper mine that occurred between 1994 and 1996 and from the Rudna copper mine that occurred between 1994
and 2004 were considered. Their source parameters and focal mechanisms were known in most cases from previous studies. Altogether
108 seismic pairs from coal mines and 118 pairs from copper mines were found, forming doublets, triplets and quadruplets,
within the magnitude range from 0.7 to 3.5. The distance and time intervals between two events forming pairs are not dependent
on magnitude of these events.
The focal mechanism of seismic events forming pairs is similar in over 60 percent of pairs at coal mines and in about one
third of pairs at copper mines. Spatial distributions of doublets in particular sections of coal and copper mines display
dominant linear trends, characteristic for a given area, which are often in conformity with the direction of nodal planes
determined by fault plane solution of one or both the events forming a doublet. In such cases, the rupture plane can be discriminated
among the nodal planes. 相似文献
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用地震反射波定量解释煤层厚度的方法 总被引:6,自引:0,他引:6
一、引言 工业可采煤层厚度一般为1.5m,如何从地震资料上准确圈定1m厚的煤层边界、并定量解释煤层厚度、准确计算地质储量,国外一些学者研究了薄层地震反射波的动力学特征与薄层厚度的关系后,得出了不同的薄层垂直分辨率标准,Widess用零相位子波作实验时,发现当薄层厚度为λ/8(λ是地震子波的主波长)时,反射波形正好是入射波的导数,并可直观地鉴别顶底反射;Kallweit利用可控震源研究了薄层响应的频谱后,提出了分辨地震波的极限为1/(1.4f)(f为地震子波的上限频率),经主频换算后,此 相似文献
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虽然煤田三维地震勘探已经过了十多年的发展,但构造解释问题仍是目前需要解决的主要问题之一.随着三维地震资料解释方法的不断发展,小波分析技术、相干体技术、地震属性技术、图像处理等提高解释精度的方法相继在地震勘探领域中得到应用.另一方面,由于煤矿采区三维地震勘探资料一般具有高信噪比和高分辨率的特点,为做好三维地震资料精细构造解释提供了物质基础.本文结合小波分析技术、相干体技术、地震属性技术等多种方法,结合两个采区的实例,对小断层和小规模陷落柱做了精细构造解释.解释结果显示联合使用以上几种解释技术,能提高三维地震资料的构造解释精度和可靠信. 相似文献
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阐述 PBS 型地震仪 CF 卡的工作原理、硬件电路接口设计及底层驱动设计,并按照 FAT32文件系统格式,实现文件存储,可方便地震记录文件在 Windows 系统下的识读,为后期数据分析与解释提供便利。 相似文献
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煤矿高产高效安全生产地质保障体系要求探明煤矿微小构造,相干体技术利用计算机分析检测三维地震数据体中相邻道之间地震信号的相似性,比常规解释方法更有利于小断层等小构造的识别;相干技术算法中C3比C1、C2两种相干算法在断层识别和边缘检测上具有更高的水平分辨率和垂直分辨率;相干体技术与地震属性技术、图象处理技术联合使用,形成煤田地震资料解释的新模式,能够更好地解决煤矿生产中遇到的构造、岩性等实际问题,极大提高三维地震成果的使用效率和应用水平;相干体技术在许厂、梁家等煤矿中应用取得了良好效果. 相似文献
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将神经网络技术用于煤田地震勘探领域,对两个矿区的实际资料进行断层检测及煤层宏观结构的解释,提高了地震资料构造解释的水平和精度。 相似文献
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The study of rock stresses and their changes is of great importance for safety in mines. To detect dangerous stress accumulations in coal mines an empirical method, Jahn's drilling test, is generally used. An experimental survey to solve the same problem by geophysical measurements was undertaken in a Hungarian coal mine. The basic idea was to determine the easily measurable seismic velocities instead of the more difficult to measure stresses in the rocks, since there is a monotonic relation between them. During the survey seismic transmission-type measurements were carried out in the fore-field of longwall faces between the top and tail roads. The seismic velocity data obtained were processed using an iterative algebraic reconstruction technique to determine the ‘velocity field’, i.e., the seismic velocity distribution, of the area covered by the ray paths. By periodically repeating the measurements in the same area, it was possible to follow the changes in the stress conditions caused by mining operations. 相似文献
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Three-component seismic and geoelectrical in-mine surveys were carried out in Lyukobanya colliery near Miskolc, Hungary to determine the in situ petrophysical parameter distributions and to detect inhomogeneities in the coal seam. The seismic measurements comprise an underground vertical seismic profile, using body waves, and an in-seam seismic amplitude-depth distribution and transmission survey, using channel waves. The geoelectrical measurements are based on the drift- and seam-sounding method. Interval traveltime-, amplitude-, multiple-filter- and polarization analysis methods are applied to the seismic data. They lead to a five-layer model for the strata including the coal seam. The coal seam and two underlying beds act as a seismic waveguide. The layer sequence supports the propagation of both normal and leaky mode channel waves of the Love- and Rayleigh type. A calculation of the total reflected energy for each interface using Knott's energy coefficients shows that the velocity ranges of high reflection energy and of normal and leaky mode wavegroups coincide. The excitation of wavegroups strongly depends on the seismic source. A simultaneous inversion of a geoelectrical drift- and seam-sounding survey prevents misinterpretations of the seismic data by clearly identifying the low-velocity coal seam as a high-resistivity bed. Calculations of dispersion and sounding curves improve the resolution of the slowness and resistivity in each layer. Both diminished amplitudes and distortions in the polarization of transmission seismo-grams and decreasing resistivities in a geoelectrical pseudosection of the coal seam are related to an inhomogeneity. A calculation of synthetic seismograms for Love and Rayleigh channel waves with the finite-difference and the Alekseev-Mikhailenko method agrees well with the field data for the main features, i.e., particular arrivals in the wave train, wavegroups, velocities and symmetries or asymmetries. This in-mine experiment demonstrates that the simultaneous acquisition, processing and interpretation of seismic and geoelectrical data improve the lithological interpretation of petrophysical parameter distributions. Coal seam inhomogeneities can also be detected more reliably by the two independent surveys than by one alone. 相似文献