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地壳垂直形变散度场与地震关系初探
引用本文:刘天铭,张伯宏,苏瑞.地壳垂直形变散度场与地震关系初探[J].高原地震,1997(4).
作者姓名:刘天铭  张伯宏  苏瑞
作者单位:国家地震局第二地形变监测中心!西安,710054,国家地震局第二地形变监测中心!西安,710054,国家地震局第二地形变监测中心!西安,710054
摘    要:用富里叶级数表示的地壳垂直形变散度计算公式,对华北、南北地震带和河西─祁连山地区的水准资料进行计算,并绘制出各时间段的等值线图。通过对各区的地震活动与地壳垂直形变散度场时空特征的分析,发现绝大多数中强地震的震中位于零散度区或其零值线附近,散度场变化越强,零值区越大,在本时间段或下一时间段内,该区的地震活动性增强。

关 键 词:重复水准测量  地壳垂直形变  应力积累  地震活动性  地震预报

PRELIMINARY STUDY ON THE RELATION OF THE DIVERGENCY FIELD DEDUCEDF ROM VERTICAL CRUSTAL DEFORMATION AND EARTHQUAKE
Liu Tianming, Zhang Bohong, Su Rui.PRELIMINARY STUDY ON THE RELATION OF THE DIVERGENCY FIELD DEDUCEDF ROM VERTICAL CRUSTAL DEFORMATION AND EARTHQUAKE[J].Plateau Earthquake Research,1997(4).
Authors:Liu Tianming  Zhang Bohong  Su Rui
Abstract:In this paper, the divergence has been computed by using the precise relevelling data ofNorth China and Hexi -Qilian area, and then mapped the divergency isogram of the area ineach period. The characteristics of earthquake activities and divergency field evolution ineach area have also been analysed thoroughly. It shows that the earthquakes always occur inthe nought divergency region. When there is a large nought divergency region in the area,there is certain strong earthquake in this region.
Keywords:Vertical crustal deformation Earthquake activity Relevelling Stress accumulation Earthquake prediction
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