价值工程
價值工程
개치공정
VALUE ENGINEERING
2014年
18期
284-285
,共2页
汶川地震%反投影%震源过程%能量辐射
汶川地震%反投影%震源過程%能量輻射
문천지진%반투영%진원과정%능량복사
Wenchuan earthquake%back-projection%earthquake focus process%energy radiation
研究中,我们从IRIS DMC搜集了震中距范围在30o-95o的欧洲台阵87个台站所记录的远震P波垂直分量,采用了IRIS提供的震源参数,首先利用IASPEI91速度模型以及几何射线方法计算出震源在震中位置时的理论走时(P波初至)进行时差校正,然后截取了P波初至前5秒和后15秒的波形记录,利用波形互相关计算出“互相关时差”并将其校正。
研究中,我們從IRIS DMC搜集瞭震中距範圍在30o-95o的歐洲檯陣87箇檯站所記錄的遠震P波垂直分量,採用瞭IRIS提供的震源參數,首先利用IASPEI91速度模型以及幾何射線方法計算齣震源在震中位置時的理論走時(P波初至)進行時差校正,然後截取瞭P波初至前5秒和後15秒的波形記錄,利用波形互相關計算齣“互相關時差”併將其校正。
연구중,아문종IRIS DMC수집료진중거범위재30o-95o적구주태진87개태참소기록적원진P파수직분량,채용료IRIS제공적진원삼수,수선이용IASPEI91속도모형이급궤하사선방법계산출진원재진중위치시적이론주시(P파초지)진행시차교정,연후절취료P파초지전5초화후15초적파형기록,이용파형호상관계산출“호상관시차”병장기교정。
This study collected the teleseismic P-wave vertical component recorded by 87 stations in Europe array whose earthquake focus is from 30oto 95ofrom the IRIS DMC, according to the earthquake focus parameters provided by IRIS, firstly used IASPEI91 speed model and geometrical ray method to calculate the travel time (P wave beginning to) when the earthquake focus in epicenter for time difference correction, then intercepted the waveform recording in first 5 seconds and after 15 seconds when P wave beginning to, and applied the waveform cross-correlation to calculate and correct the"cross-correlation difference".