地下水气对现今地球表层动力过程的响应及其意义  

RESPONSE OF UNDERGROUND WATER AND GAS TO MODERN DYNAMIC PROCESSES OF EARTH SURFACE LAYER AND ITS SIGNIFICANCES

作　　者：张培仁[1] 车用太[1] 王基华[1] 朱清钟[1] 

机构地区：[1]国家地震局地质研究所

出　　处：《地球科学（中国地质大学学报）》1998年第1期107-110,共4页Earth Science-Journal of China University of Geosciences

基　　金：地震科学联合基金

摘　　要：以新近取得的地下水气动态观测资料为基础，提出地下水气不仅是物质资源，同时又是重要的信息资源，其动态对现今地球表层动力过程的响应具有很高的灵敏性和很宽的频带特性．地下水气动态的观测与研究不仅有助于人类把握现今地球表层动力过程的规律，预测预报地壳构造运动，而且对于预测自然环境变化与灾害等方面也有重要意义．Based on the recent observations of underground water and gases, it is suggested that underground waters and gases are not only material but also important information resources, and that the response of their behavior to some modern dynamic processes of earth surface layers have higher sensitivity and wider spectrum. Therefore, the monitoring and studies of underground waters and gases are of greater significance in predicting crust tectonic movement and some natural environment disasters.

关 键 词：地下水气 地球动力过程 地球表层 地震预报 

分 类 号：P315.7[天文地球—地震学] P541[天文地球—固体地球物理学]