中国大陆地震活动高潮期与平静期水化学变化特征及其意义的研究
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地震科学联合基金


STUDY ON THE CHARACTERISTICS OF HYDROCHEMICAL CHANGE DURING THE HIGH AND LOW SEISMICITY PERIODS ON CHINA CONTINENT
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    摘要:

    本文根据对华北、南北地震带等大范围内20多个(总共约40个)主要水化学(水氡)观测点近20年连续变化曲线的分析,发现1966-1976年地震活动高潮期均呈现趋势性高值异常,突变异常比较普遍。1977-1985年地震活动相对平静期则呈现平稳的正常值变化,只是在局部地区的个别测点出现短趋势异常或突变异常。由此认为地震活动高潮期大区域应力场作用下形成大范围水化学异常场,这是预报连发性大震的一个重要标志。

    Abstract:

    In terms of analysis on the continuous change curves of radon in groundwater at more than twenty measuring points along the north China and North-South tectonic belt,it is found that the tendenciously high value anomaly and abrupt anomaly were common during the high seismicity period from 1966 to 1976.But during the low seismicity period from 1977 to 1985,the groundwater radon value is stable except the short-term tendency anomaly or abrupt anomaly at few points in local area,It is considered that the hydrochemical anomaly field under the action of the regional stress field during high seismicity period is an important indication for the prediction of one-by-one strong events.

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张文冕,倪明康,陶淑芬,张佩山,姚军.中国大陆地震活动高潮期与平静期水化学变化特征及其意义的研究[J].地震工程学报,1995,17(3):43-47. Zhang Wenmian, Ni Mingkang, Tao Shfen, Zhang Peishan, Yao Jun. STUDY ON THE CHARACTERISTICS OF HYDROCHEMICAL CHANGE DURING THE HIGH AND LOW SEISMICITY PERIODS ON CHINA CONTINENT[J]. China Earthquake Engineering Journal,1995,17(3):43-47.

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  • 收稿日期:1994-09-29
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  • 在线发布日期: 2017-06-30