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中心回线瞬变电磁探测的一种快速解释方法
引用本文:郭文波,宋建平,韩俊明,曹捷,李正宇.中心回线瞬变电磁探测的一种快速解释方法[J].物探与化探,2006,30(2):154-157,161.
作者姓名:郭文波  宋建平  韩俊明  曹捷  李正宇
作者单位:1. 西安交通大学,电信学院,陕西,西安,710049;西北有色地质勘查局物化探总队,陕西,西安,710068
2. 西安交通大学,电信学院,陕西,西安,710049
3. 西北有色地质勘查局712总队,陕西,咸阳,712000
4. 西北有色地质勘查局物化探总队,陕西,西安,710068
5. 长安大学,陕西,西安,710054
摘    要:分析了中心回线装置激发的电磁场在晚期与平面电磁波的传播特征,通过时-频转换将TEM数据转换成平面波场数据,构建了关于反射函数的M×N阶欠定方程组。用线性规划法解出反射函数序列qm,大量模型的反演结果与理论值误差很小。以qm为参数绘制出电磁响应时间剖面图,从而实现了TEM快速成像解释。成像剖面清楚地反映了断面的地电特征。实测资料的处理结果说明了方法的实用性。

关 键 词:瞬变电磁法  中心回线装置  电磁成像  解释方法
文章编号:1000-8918(2006)02-0154-04
收稿时间:2005-10-10
修稿时间:2005-10-10

A NEW RAPID INTERPRETATION METHOD FOR CENTRAL-LOOP-SOURCE TRANSIENT ELECTROMAGNETIC DETECTION
GUO Wen-bo,SONG Jian-ping,HAN Jun-ming,CAO Jie,LI Zheng-yu.A NEW RAPID INTERPRETATION METHOD FOR CENTRAL-LOOP-SOURCE TRANSIENT ELECTROMAGNETIC DETECTION[J].Geophysical and Geochemical Exploration,2006,30(2):154-157,161.
Authors:GUO Wen-bo  SONG Jian-ping  HAN Jun-ming  CAO Jie  LI Zheng-yu
Institution:1. School of Electronic &; Information Engineering, Xi'an Jiaotong University, Xi'an 710049, China;
2. Geophysical and Geochemical Exploration Party, Northwest Bureau of Geological Exploration for Nonferrous Metals, CNNC, Xi'an 710068, China;
3. No. 712 Geological Party, Northwest Bureau of Geological Exploration for Nonferrous Metals, CNNC, Xianyang 712000, China;
4. School of Geology and Survey, Changan University, Xi'an 710054, China
Abstract:The central-loop device is an important surveying means for transient electromagneticmethod. It is necessary to make a rapid interpretation and improve the interpretation level. The electromagnetic field stimulated by the central-loop-source in the late period is similar to the plane-electromagnetic-wave. Through the time-frequency conversion, the TEM data are transformed to the plane-wave field data, thus constructing the system of M×N order underdetermined equations related to the reflection function. The authors have designed a computer programme to solve the reflected function sequence qm with the method of Linear programming, and the error between the inversion result of a host of models and the theoretical value is very small, which indicates this method is feasible and the calculation result is correct. The electromagnetic response time-section is drawn with the parameter qm, which realizes the explanation of the TEM rapid imaging. The imaging section clearly reflects the geoelectric characteristics of the section. The processing results of the field data demonstrate that this method is useful and practical.
Keywords:central-loop-source  transient electromagnetic method  electromagnetic wave  reflected function  tomography
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