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Development of an on-site Data Processing System-and-Application Soft for Reconnaissance Survey to Estimate Deep Geological Structure Using Microtremors

Development of an on-site Data Processing System-and-Application Soft for Reconnaissance Survey to Estimate Deep Geological Structure Using Microtremors
开发利用微震估算深层地质结构的勘察现场数据处理系统和应用软件
批准号:
07555321
负责人:
OKADA Hiroshi
金额:
$10.18万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for Scientific Research (A)
财政年份:
1995
资助国家:
日本
项目状态:
已结题
起止时间:
1995 至 1997

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中文摘要
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英文摘要
The fundamental programs and system-and-application softs have been developed for easy and quick data-processing for a new exploration technique which makes use of microtremors observable at any time in any place with a fairly stable spectrum. The technique can estimate geologic structure in a form of S-wave velocity distribution down to a depth of about 3km from measuring phase velocities of surface waves (Rayleigh waves) in microtremors with periods longer than Is, by observing with a seismic array consisting of 7 to l0 seismometers.The data processing in the technique includes estimating power spectra and cross spectra. For the measurement of phase velocities of surface waves, frequency-wavenumber power spectral densities (F-K spectra) for the F-K method, and spatial autocorrelation coefficients (SPAC coefficients) for the SPAC method are calculated from microtremor data observed. The phase velocities of surface waves are then inverted to an S-wave velocity distribution by an inversion technique.All the fundamental programs and application softs required with these data processing are included in the newly developed application soft 'BIDOU', in which the theoretical phase velocities of either Rayleigh or Love waves for a structure model are also available.A cross section of profile withspatially placed sites where seismometer arrays are deployed and geologic structures are determined is also given by S-wave velocity versus depth distribution, for which the soft program 'DANMEN' has been developed. The program 'DANMEN' can link with respective layrs for S-wave velocities determined under the sites where arrays are deployed.These developed programs and softs are fully integrated data acquisition and processing for a new exploration technique using microtremors, operating in Widows 3.1 on PC.These powerful programs and softs have been tested at more than 50 sites where good results have been obtained.
期刊论文(9)
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会议论文
村山 隆平: "格子上受振点展開を用いた3次元コヒーレンドノイズの観測" 物理探査. 49. 372-386 (1996)
Ryuhei Murayama:“使用网格上的接收点扩展观察三维相干噪声”物理探索 49. 372-386 (1996)。
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森谷 武男: "位相誤差の少ない微動探査の観測法" 物理探査. 49. 210-217 (1996)
Takeo Moriya:“相位误差较小的微震勘探观测方法”《物理调查》49. 210-217 (1996)。
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凌 甦群: "微動中の表面波と地震動による表面波の推定と比較" 北海道大学地球物理学研究報告. 61. 115-132
凌书官:《地震时面波与地震运动引起的面波的估计与比较》北海道大学地球物理研究报告61. 115-132。
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