共查询到19条相似文献,搜索用时 109 毫秒
1.
在开发地震目录查询系统的过程中,通过CSS样式和PHP程序的结合运用。可动态地控制地震目录查询系统的返回结果,使查询结果的显示可以随获取的地震目录的条数而改变。极大地方便查询者。 相似文献
2.
3.
4.
SeisMIS地震管理信息系统是一个建立在Linux Oracle平台上,可以提供以单个地震事件为核心的综合性地震数据服务的系统。建设该系统的目的是为了能够更好地管理和应用现有的SEED格式的地震事件数据。这篇文章阐述了SeisMIS系统的设计方案,重点介绍了SeisMIS系统的数据查询、数据服务以及数据库管理功能的实现方式。 相似文献
5.
历史地震图数据库及共享平台 总被引:1,自引:1,他引:0
历史地震图纸是记录历史地震的重要资料,在进行电子化之前,图纸的唯一性限制了其大范围共享的可能。电子化处理是抢救和保护历史地震图纸的重要手段,可以有效发挥其使用及研究价值,具有重要意义。为此研制历史地震图数据库及共享平台,对北京国家地球观象台现存的60万张历史地震图纸进行高精度(600 dpi)扫描和规则化命名,利用数据库和FastDFS分布式文件系统进行统一存储,并采用多级缩略图和网络服务方式提供数据共享服务。 相似文献
6.
7.
8.
开发了福建数字地震台网的一个地震编目系统,该系统具有如下功能直接使用人机交互分析处理系统输出的地震定位结果文件,对地震目录和观测报告数据库进行自动更新;多种格式地震目录和观测报告文件的输出;在矢量地图上进行点查询与区域查询等。本文就该系统的概况、特点及开发技术予以介绍。 相似文献
9.
基于国家台网地震速报的实际工作需求,针对国家台网在全球地震速报中缺乏专门的地名查询系统,通过对国家台网实时、人机交互处理子系统和全国速报信息交换平台(EQIM系统)的相关协议和数据接口进行研究,并结合地震速报相关规定中对地名的要求,基于地理信息系统Arc GIS提供的Arc GIS Engine(AE)组件技术,采用Visual.Net开发平台和COM组件技术,来实现获取地震地名信息的功能,开发设计一套用于国家台网地震速报的地名查询辅助系统,希望可以有效提高国家台网地震速报的效率和准确度。 相似文献
10.
地震数据资源信息远程管理系统是为管理和更新地震数据资源信息而设计的。提供数据资源信息的各个单位都可以通过该系统远程动态更新地震数据资源信息服务系统的资源信息库。为确保数据信息的安全性,该系统应该具有两种功能:权限管理和远程动态更新信息。系统管理员对不同的用户授予不同的权限,用户在输入密码后得到验证,方可进入该系统。每个用户通过浏览器只能看到自己权限内的数据,并对数据进行入库、查询、修改。本系统采用目前流行的S/B结构,运用JSP和Java语言来实现系统功能。 相似文献
11.
地震台站地震图管理系统设计及实现 总被引:1,自引:1,他引:0
根据我国地震观测台站的实际需要,设计一个通用地震图管理系统。系统采用ACCESS设计数据库,VB6.0开发管理软件,具有显示、管理、打印和查询等多种功能,可以用来编制电子地震图集和管理地震图,在一定程度上解决了堆积如山的模拟地震图与数字地震观测数据的管理和利用问题,并为互联网地震数据共享打下基础。 相似文献
12.
CDSN台站典型震例数字地震图库的建立 总被引:2,自引:2,他引:0
主要描述利用UNIX的SHELL组合命令实现数字地震图库的建立。图库按时间顺序排列,地震波形文件与数据库中相关的表(TABLE)分开存放,波形文件是以CSS3.0格式存储的,符合ARS的使用习惯。使用时用户只需更改数据库的名字,即可使用功能很强的ARS分析软件,对数字地震图进行回放处理等操作 相似文献
13.
IntroductionSeismograms contain seismic wave data recorded by instruments. They are the main information source for seismological studies. Now we are developing seismological stations with digital records, which can offer seismic wave data with better quality than before. But the paper analog seismograms accumulated in the past decades still have great room for application. They are important original data for studying earthquakes. Lots of valuable information are contained in them. Due to a… 相似文献
14.
Bagus Jaya Santosa 《中国地震研究》2009,23(2):210-222
The S-wave velocity across the earth structure under Indonesia for Indonesia earthquakes has been investigated through seismogram analysis, simultaneously in the time domain and three Cartesian components. The data were recorded at DAV observational station, the Philippines. The main data set is the seismogram comparison between the measured and synthetic seismogram, instead of travel time data, as commonly used in other seismological research. The synthetic seismogram is calculated using the GEMINI method, which is equivalent to Mode Summation. The above seismogram comparison shows that the global earth mantle of PREMAN gives a deviating synthetic seismogram and has earlier arrival times than those of the measurement. The gradient of β_h in the upper mantle layers is altered into a positive, rather than negative slope as stated in the PREMAN model, and negative corrections are imposed to the zero order of the polynomials coefficients in all earth mantle layers. The excellent fitting, as well as travel time or waveform, is obtained from the surface waves of Love and Rayleigh, surface wave to the S and SS mantle waves as well as the core reflected waves. This result expresses that part of the earth mantle, due to a collision between India and Asia tectonic released zones, has a negative anomaly in S-wave velocity and vertical anisotropy in all of the earth mantle layers. 相似文献
15.
E. SZARANIEC 《Geophysical Prospecting》1984,32(5):812-818
In odd-depth structure the two-way traveltime to each boundary is constrained to be an odd integer. The odd-depth property of a model is exposed to possible refutation under a seismogram test. Test function is a simple transformation of a synthetic seismogram. For an odd-depth model the test function has identically the value 1. The testability of a synthetic seismogram over an odd-depth structure provides a method of deterministic deconvolution. There is no need of specialized assumptions, like the minimum-phase property, about the source wavelet. The deconvolution may be performed in the absence of the early segment of a seismogram. 相似文献
16.
17.
18.
19.
We propose a wave scattering approach to the problem of deconvolution by the inversion of the reflection seismogram. Rather than using the least-squares approach, we study the full wave solution of the one-dimensional wave equation for deconvolution. Randomness of the reflectivity is not a necessary assumption in this method. Both the reflectivity and the section multiple train can be predicted from the boundary data (the reflection seismogram). This is in contrast to the usual statistical approach in which reflectivity is unpredictable and random, and the section multiple train is the only predictable component of the seismogram. The proposed scattering approach also differs from Claerbout's method based on the Kunetz equation. The coupled first-order hyperbolic wave equations have been obtained from the equation of motion and the law of elasticity. These equations have been transformed in terms of characteristics. A finite-difference numerical scheme for the downward continuation of the free-surface reflection seismogram has been developed. The discrete causal solutions for forward and inverse problems have been obtained. The computer algorithm recursively solves for the pressure and particle velocity response and the impedance log. The method accomplishes deconvolution and impedance log reconstruction. We have tested the method by computer model experiments and obtained satisfactory results using noise-free synthetic data. Further study is recommended for the method's application to real data. 相似文献