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Annual Report 2000 - WIT

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Ý<br />

ã<br />

ä<br />

and ã<br />

with the slowness vectors at ã äñ<br />

and ã î§ñ<br />

Þ<br />

§<br />

ò<br />

䨥 §<br />

¤ ¦<br />

©©©©©<br />

û<br />

ã<br />

ã<br />

Ý<br />

. The Taylor expansion for ò æ ã ä¡ê ã<br />

î<br />

þ ã<br />

§<br />

ò<br />

î¥ §<br />

The second order derivatives are given by the ã þ<br />

matrices<br />

ã þ ¥qå<br />

Þ<br />

§<br />

ä¥ § ä §<br />

<br />

©©©©©<br />

ê<br />

§<br />

î¥ § î¨ §<br />

ý<br />

<br />

©©©©©<br />

û<br />

ã<br />

,<br />

*<br />

Ý<br />

¤ <br />

©©©©©<br />

ã , ã<br />

û<br />

and<br />

ã<br />

û ¥qå<br />

Ý<br />

Þ<br />

<br />

§<br />

ä¥ § î¨ §<br />

Ý<br />

<br />

©©©©©<br />

<br />

ä<br />

205<br />

panded into a Taylor series until second degree. Provided that the distance to the<br />

expansion point is small, the Taylor series yields a good approximation for the original<br />

traveltime function. The size of the vicinity describing 'small' distances depends on<br />

the scale of velocity variations in the input model.<br />

For the 3-D case, the Taylor expansion has to be carried out in 6 variables: the 3<br />

components of the source position ã vector<br />

äÒåçæèä§égê ä<br />

ê äë ìí<br />

and those of the receiver<br />

position ã<br />

ê×î ê×î§ë ì í<br />

. The values of ã ä<br />

and ã î<br />

in the expansion point are ã äñ<br />

and ã î§ñ<br />

îåïæðîé<br />

with the ò ñ<br />

traveltime ã äñ<br />

from ã to<br />

ó¿ã and<br />

to second order is<br />

î<br />

are such that ã<br />

äñõô óµã<br />

î§ñNô ó¿ã<br />

. The variations in source and receiver positions óµã<br />

î§ñ<br />

up<br />

îZì<br />

ä„å<br />

îzå<br />

ó¿ã äÿô<br />

ý óqã î í ã ó¿ã î ô¢¡æ¤£©ì<br />

(1)<br />

ü<br />

ò æ ã ä©ê ã îZìöå<br />

ò ñ Þ÷ã øùñ óµã äÎô<br />

ú²ñ óqã î Þµóµã ä í<br />

ã<br />

î Þ‚ü ý óµã ä í<br />

óqã<br />

(2)<br />

ú²ñ¦¥õå<br />

øùñ¦¥å<br />

with<br />

(3)<br />

Ý ò<br />

Ý ò<br />

Ý ò<br />

ã ¥¿å<br />

<br />

Equation (1) describes the parabolic traveltime expansion.<br />

Since we know that diffraction traveltimes can be expressed by hyperbolae rather then<br />

by parabolae (e.g., (Ursin, 1982), (Schleicher et al., 1993)) we will now derive a hyperbolic<br />

expression for ò æ ã<br />

îZì<br />

we expand its square,<br />

ò Ý æ ã ä©ê ã<br />

ã îZì<br />

. Instead of expanding ò æ ã äê ã<br />

ä©ê<br />

, again until second order. Applying the chain rule and the abbreviations (2)<br />

îZì<br />

and (3) leads to<br />

ò Ý æ ã ä©ê ã îZìå<br />

æ ò ñ Þ’ã ø•ñ ó¿ã ä•ô<br />

ú€ñ ó¿ã îZì Ý ô ã<br />

ò ñ! Þ<br />

óµã ä í<br />

î Þ—ó¿ã ä í ã þ<br />

óµã äô ó¿ã<br />

óqã î í ã óqã î#" ô$¡Òæ%£¡ì<br />

(4)<br />

<br />

This equation is the hyperbolic traveltime expansion. The same result (4) can be obtained<br />

by squaring equation (1) and neglecting any terms of higher spatial order than<br />

two, corresponding to a Taylor expansion of (1). This approach was used by (Schleicher<br />

et al., 1993). Please note that for the derivation of (1) and (4) no assumption on<br />

the model was made. Therefore these expressions not only apply to 3-D heterogeneous<br />

media but even to anisotropic media.<br />

A similar result for reflection traveltimes was presented by (Ursin, 1982) and (Gajewski,<br />

1998). Gajewski considers a CMP-situation &ðã ä & å Þ'& ã î & å)(<br />

with as half offset<br />

coordinate for a laterally homogeneous layered medium. Using the zero offset ray and<br />

leads to<br />

ã å Þ ã þ<br />

ý ò ñ ã<br />

û+*<br />

ü<br />

(5)<br />

ò Ý å<br />

ò Ý ñ ô<br />

Ý å<br />

ò Ý ô<br />

-/.10

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