NONCAUSALITY OF THE DISCRETE-TIME MAGNETOTELLURIC IMPULSE-RESPONSE

被引:17
作者
EGBERT, GD
机构
关键词
D O I
10.1190/1.1443204
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
For the most part, MT data processing and interpretation is best accomplished in the frequency domain. However, for some purposes estimates of the time-domain DTIR can be useful. When input signals are restricted to appropriately band-limited functions, there is always a well defined DTIR that produces the same outputs as the continuous time counterpart. However, causality of the DTIR does not follow from causality of the CTIR, and forcing a DTIR estimated from frequency-domain impedance measurements to be causal can lead to very poor results. In some circumstances (e.g., the 1-D MT problem), the CTIR is known to be causal. For computing smooth transfer functions which interpolate frequency-domain estimates, one would perhaps like to enforce this constraint. This can be done in a number of ways, but not by forcing zn = 0 for n < 0 in the expansion of equation (8). -from Author
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页码:1354 / 1358
页数:5
相关论文
共 13 条
[11]  
WIELADEK R, 1977, PUBL I GEOPHYS POL G, V1, P3
[12]   THE RECONSTRUCTION OF THE MAGNETOTELLURIC IMPEDANCE TENSOR - AN ADAPTIVE PARAMETRIC TIME-DOMAIN APPROACH [J].
YEE, E ;
KOSTENIUK, PR ;
PAULSON, KV .
GEOPHYSICS, 1988, 53 (08) :1080-1087
[13]  
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