摘要Based on analyses of the spatio-temporal evolutionary characteristics of teleseismic response recorded by Fujian subsurface fluid network and in combination with earthquakes happened in Fujian province during the same period, this paper points out that the step-like rising of water level after distant earthquakes may include some regional stress field information, and the area where water level step-like rises could be the position that the stress concentrated on and where the future earthquakes would occur. If combined with other impending precursors, the location of the events may be predicted to a certain degree.
Abstract：Based on analyses of the spatio-temporal evolutionary characteristics of teleseismic response recorded by Fujian subsurface fluid network and in combination with earthquakes happened in Fujian province during the same period, this paper points out that the step-like rising of water level after distant earthquakes may include some regional stress field information, and the area where water level step-like rises could be the position that the stress concentrated on and where the future earthquakes would occur. If combined with other impending precursors, the location of the events may be predicted to a certain degree.
基金资助:the project from China Earthquake Administration, the Chinese National Science and Technology Program (2006BAC01B02-03-02) and the foundation from Administration Earthquake of Fujian province (200801)
通讯作者:
Lixia Liao
E-mail: redllx@tom.com
引用本文:
Lixia Liao, Xiaoyin Ni, Meiling Wang, Shaozu Wu. Coseismic effects recorded by Fujian subsurface fluid network and its meaning to earthquake prediction[J]. 《地震学报》英文版, 2009, 22(3): 293-299.
Lixia Liao, Xiaoyin Ni, Meiling Wang, Shaozu Wu. Coseismic effects recorded by Fujian subsurface fluid network and its meaning to earthquake prediction. Earthquake Science, 2009, 22(3): 293-299.
