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固体潮潮汐因子的空间分布特征与机理
引用本文:唐九安,常千军,杜锡武,王川华.固体潮潮汐因子的空间分布特征与机理[J].大地测量与地球动力学,1997(1).
作者姓名:唐九安  常千军  杜锡武  王川华
作者单位:国家地震局兰州地震研究所,河北省地震局
基金项目:国家地震局地震科学联合基金
摘    要:基于O1波与K1波和M2波潮汐因子的比值,介绍了我国南北地震带及华北等地区9个重力台站(10套重力仪)、10个静水位井、11个倾斜及线应变台站潮汐因子的空间分布特征。与莫氏地球模型对比,重力线应变和水位潮汐中,O1波与K1波潮汐因子的比值均显示了液态地核的振荡效应。倾斜固体潮中,潮汐因子(特别是NS向)受局部构造环境影响畸变严重

关 键 词:固体潮  潮汐因子

SPATIAL DISTRIBUTION CHARACTERISTIC OF EARTH TIDES AND ITS MECHANISM
Abstract:In this paper, the spatial distribution characteristic of earth tides in the area of North-South Seismic Belt and North of China etc, including 9 stations of 10 set gravimeters, 10 stations of water level well and 12 tilt and line strain stations, is introduced. Comparing the results of gravity line strain and water level well with that of the theoretical value of Molodensky's Earth Model,the factors of O 1 / K 1 show obviously the dynamic effect of the liguid-state earth core. The observational results of tilt tides, especially north-south direction,are disturbed seriously by the geological structure environment near the stations.
Keywords:earth tide  tidal factor
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