内陆地震
內陸地震
내륙지진
INLAND EARTHQUAKE
2009年
2期
107-115
,共9页
杨又陵%马世贵%李晓东%哈斯高娃
楊又陵%馬世貴%李曉東%哈斯高娃
양우릉%마세귀%리효동%합사고왜
数字化形变观测%潮汐参数%精度%稳定性
數字化形變觀測%潮汐參數%精度%穩定性
수자화형변관측%조석삼수%정도%은정성
Digital deformation observation%Tidal parameters%Accuracy%Stability
利用潮汐分析的方法,分析和评价了新疆数字化形变观测资料的精度和稳定性.结果表明,主波M2波、O1波的潮汐因子的纬度分布与理论值有较好的一致性,中误差小;各台仪器的观测精度达到并超过了中国地震局形变Ⅰ类台的标准;地倾斜类观测仪器精度高,稳定性好,尤其是水管倾斜仪的各项指标普遍高于其他类仪器,mγ<0.005;硐体应变仪的δα/α<0.03,体应变仪的δα/α<0.01,超过δα/α<0.05的指标.研究还发现,个别台站仪器定向和方位角存在较大偏差.
利用潮汐分析的方法,分析和評價瞭新疆數字化形變觀測資料的精度和穩定性.結果錶明,主波M2波、O1波的潮汐因子的緯度分佈與理論值有較好的一緻性,中誤差小;各檯儀器的觀測精度達到併超過瞭中國地震跼形變Ⅰ類檯的標準;地傾斜類觀測儀器精度高,穩定性好,尤其是水管傾斜儀的各項指標普遍高于其他類儀器,mγ<0.005;硐體應變儀的δα/α<0.03,體應變儀的δα/α<0.01,超過δα/α<0.05的指標.研究還髮現,箇彆檯站儀器定嚮和方位角存在較大偏差.
이용조석분석적방법,분석화평개료신강수자화형변관측자료적정도화은정성.결과표명,주파M2파、O1파적조석인자적위도분포여이론치유교호적일치성,중오차소;각태의기적관측정도체도병초과료중국지진국형변Ⅰ류태적표준;지경사류관측의기정도고,은정성호,우기시수관경사의적각항지표보편고우기타류의기,mγ<0.005;동체응변의적δα/α<0.03,체응변의적δα/α<0.01,초과δα/α<0.05적지표.연구환발현,개별태참의기정향화방위각존재교대편차.
The tide analysis method was used to analyze and assess the accuracy and stability of digital deformation observation in Xinjiang.The results showed there was better consistency between the latitude distributions of main wave tidal factor and theoretical value, and the quadratic mean deviation was very small. The observation accuracy of all observation instruments met or surpassed the standard of class 1 deformation stations of China Earthquake Administration. The observation instruments of ground tilt have higher accuracy and better stability; especially all the indices of water tube inclinometer are higher than other type of instruments. The study indicated there was obvious deviation in the determination of direction and azimuth in several stations.