高原地震
高原地震
고원지진
EARTHQUAKE RESEARCH IN PLATEAU
2011年
4期
31-36
,共6页
张志慧%王帅合%李亚军%董晓娜%李霞%山长仑
張誌慧%王帥閤%李亞軍%董曉娜%李霞%山長崙
장지혜%왕수합%리아군%동효나%리하%산장륜
峰值加速度%环境剪应力值%山东数字地震台网
峰值加速度%環境剪應力值%山東數字地震檯網
봉치가속도%배경전응력치%산동수자지진태망
Seismic peak ground acceleration%Environment shear stress%Seismological digital seismic network of Shandong province
利用山东数字地震台网记录资料,根据陈培善等用地震发生的断裂力学模式和震源谱理论,导出的震源处峰值加速度与构造环境剪应力值的关系,计算了山东长岛地区发生的中小地震构造环境剪应力值,并对应力场的分布状况和时空变化进行了分析。结果表明:剪应力τ值随矩震级(ML)的增大而增大,对两者作拟合得到它们之间较简单的关系为:τ=1.89 ML-1.76。在所研究的区域范围内,其构造环境剪应力τ值为1.0~6.0兆帕,与陈培善对3.0~5.5级地震的τ值多在4~8兆帕之间这一统计结果基本一致。
利用山東數字地震檯網記錄資料,根據陳培善等用地震髮生的斷裂力學模式和震源譜理論,導齣的震源處峰值加速度與構造環境剪應力值的關繫,計算瞭山東長島地區髮生的中小地震構造環境剪應力值,併對應力場的分佈狀況和時空變化進行瞭分析。結果錶明:剪應力τ值隨矩震級(ML)的增大而增大,對兩者作擬閤得到它們之間較簡單的關繫為:τ=1.89 ML-1.76。在所研究的區域範圍內,其構造環境剪應力τ值為1.0~6.0兆帕,與陳培善對3.0~5.5級地震的τ值多在4~8兆帕之間這一統計結果基本一緻。
이용산동수자지진태망기록자료,근거진배선등용지진발생적단렬역학모식화진원보이론,도출적진원처봉치가속도여구조배경전응력치적관계,계산료산동장도지구발생적중소지진구조배경전응력치,병대응력장적분포상황화시공변화진행료분석。결과표명:전응력τ치수구진급(ML)적증대이증대,대량자작의합득도타문지간교간단적관계위:τ=1.89 ML-1.76。재소연구적구역범위내,기구조배경전응력τ치위1.0~6.0조파,여진배선대3.0~5.5급지진적τ치다재4~8조파지간저일통계결과기본일치。
Based on the digital observation data recorded by the seismological digital seismic network of Shan-dong Province, rupture mechanics model and seismic focus theory by CHEN Peishan, this paper educes the relation between peak value acceleration and structural shearing stress value, calculates the stress value from earthquakes occurred in Changdao area, and analyzes the time and space distribution characteristics of stress field. The resuh shows that the shear stress r is increasing with the moment magnitude ML, and by fitting r and ME, the authors can get the simple relationship between them, that is r = 1.89 ML - 1- 76. In the study area, the tectonic ambient shear stress r is between 1.0 to 6. 0 MPa. It is consistent with the results in Chen Peishan' s article, which shows that the r value is between 4 to 8 MPa which magnitudes are 3.0 to 5.5.