INSTANTANEOUS FREQUENCY AND AMPLITUDE AT THE ENVELOPE PEAK OF A CONSTANT-PHASE WAVELET

被引:45
作者
BARNES, AE
机构
[1] CORNELL UNIV,INST STUDY CONTINENTS,ITHACA,NY 14853
[2] CORNELL UNIV,DEPT GEOL SCI,ITHACA,NY 14853
关键词
D O I
10.1190/1.1443115
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Robertson and Nogami (1984) have shown that the instantaneous frequency at the peak of a zero-phase Ricker wavelet is exactly equal to that wavelet's average Fourier spectral frequency weighted by its amplitude spectrum. Bodine (1986) gave an example which shows this is also true for constant-phase bandpass wavelets. Here it is shown that this holds for any constant-phase wavelet. An equation is developed depressing this quantity as a function of propagation time through an attenuating medium. A corresponding equation is derived for the amplitude of the envelope peak. -from Author
引用
收藏
页码:1058 / 1060
页数:3
相关论文
共 9 条
[1]  
BARNES AE, 1990, 60 ANN INT M SOC EXP, P1553
[2]  
BODINE JH, 1986, OIL GAS J, V84, P59
[3]  
Claerbout J.F., 1985, IMAGING EARTHS INTER
[4]   COMPLEX SEISMIC TRACE ANALYSIS OF THIN BEDS [J].
ROBERTSON, JD ;
NOGAMI, HH .
GEOPHYSICS, 1984, 49 (04) :344-352
[5]  
ROBERTSON JD, 1988, LEADING EDGE, V7, P22, DOI DOI 10.1190/1.1439517
[6]  
SAHA JG, 1987, 57TH ANN INT M SOC E, P591
[7]  
Sheriff R.E, 1984, ENCY DICT EXPLORATIO
[8]   COMPLEX SEISMIC TRACE ANALYSIS [J].
TANER, MT ;
KOEHLER, F ;
SHERIFF, RE .
GEOPHYSICS, 1979, 44 (06) :1041-1063
[9]  
Toksoz M. N., 1981, SEISMIC WAVE ATTENUA