核磁共振测深方法的新进展  

New progress of Magnetic Resonance Sounding (MRS)Method—A Record of Events of Taking Part in the 2nd MRs International Workshop

作　　者：李振宇[1] 高秀花[2] 潘玉玲[1] 

机构地区：[1]中国地质大学(武汉)地球物理与空间信息学院,武汉430074 [2]中国地质大学(北京)水资源与环境工程学院,北京100083

出　　处：《CT理论与应用研究（中英文）》2004年第2期6-10,共5页Computerized Tomography Theory and Applications

摘　　要：核磁共振测深(MRS)方法是目前唯一直接探查地下水的新方法。本文概要介绍了参加第二届核磁共振测深(MRS)国际学术研讨会的主要收获。阐述了核磁共振找水仪的研制和进展以及扩大了MRS方法的应用领域方面的情况。在应用MRS方法探测地下水取得很大成效的此基础上,我们率先用MRS方法进行了三峡滑坡监测和秦始皇陵考古工作,又取得了新成果。Magnetic Resonance Sounding (MRS) is the only geophysical new method of directly detecting underground water at present. In this paper the main gains of taking part in the 2nd MRS international workshop are introduced, development and progress of hydroscope and applications of MRS method are considered. On the basis of the MRS successful application in the detection of underground water, using MRS method new progress has been made in slide monitoring of Three Gorges and archeology of the first Qin dynasty imperator mausoleum for the first time.

关 键 词：核磁共振测深 国际学术研讨会 滑坡监测 考古 

分 类 号：P631.6[天文地球—地质矿产勘探]