DISTURBANCE CHARACTERISTICS OF CAVE STRAIN OBSERVATIONCAUSED BY SEA TIDE AT XIAMEN SEISMOSTATION
Xiong Xianbao 1) ;Lin Chunmei 2) ; Huang Xiaohua 1) ;1) ;Huang Chaohui 2) ; Lin Lifeng 1) ; and Xu Zhiming 1)
1) Xiamen Seismostation,Earthquake Administration of Fujian Province, Xiamen 3610032) Xiamen Ocean Environment Monitoring Station, China Ocean Administration, Xiamen 361002
Abstract By contrasting the geo-deformation materials observed at Xiamen station with that at the inland seismostations and excluding a variety of possible disturbing factors on cave strain materials, it is found that lots of “burr” and another hig-frequency phenomenon which superpose on the solid tide observation curves are caused by sea tide surge movement. Different from the observations of ground tilt instruments, the type of sea tide disturbance on cave strain observation is belong to vibration type.
Key words ：
disturbance characteristic
disturbance type
sea tide
cave strain observation
Xiamen seismostation
Received: 01 January 1900
Cite this article:
Xiong Xianbao ,Lin Chunmei ,Huang Xiaohua et al. DISTURBANCE CHARACTERISTICS OF CAVE STRAIN OBSERVATIONCAUSED BY SEA TIDE AT XIAMEN SEISMOSTATION[J]. , 2010, 30(Supp.1): 33-37.
Xiong Xianbao ,Lin Chunmei ,Huang Xiaohua et al. DISTURBANCE CHARACTERISTICS OF CAVE STRAIN OBSERVATIONCAUSED BY SEA TIDE AT XIAMEN SEISMOSTATION[J]. jgg, 2010, 30(Supp.1): 33-37.
URL:
http://www.jgg09.com/EN/ OR http://www.jgg09.com/EN/Y2010/V30/ISupp.1/33
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