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Annual Report 2000 - WIT

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Š<br />

Š<br />

Æ<br />

³<br />

Š<br />

» •ÌÃ)Í<br />

½<br />

Í<br />

³<br />

¢¢¢¢¢ÏÎ<br />

Î<br />

Æ ¿ ‘ • Í » ³ ½ ¿ ³ ¢ Í ¢¢¢¢Î<br />

Î<br />

Ç<br />

Š<br />

Š<br />

221<br />

Vanelle, C., and Gajewski, D., <strong>2000</strong>b, Traveltime based true amplitude migration: 70th<br />

Ann. Internat. Mtg., Soc. Expl. Geophys., Expanded Abstracts, 961–964.<br />

Vanelle, C., and Gajewski, D., <strong>2000</strong>c, True-amplitude migration weights from traveltimes:<br />

PAGEOPH (submitted).<br />

Vidale, J., 1990, Finite-difference calculation of traveltimes in three dimensions: Geophysics,<br />

55, 521–526.<br />

PUBLICATIONS<br />

Previous results concerning true-amplitude migration were published by (Vanelle and<br />

Gajewski, <strong>2000</strong>b) and (Vanelle and Gajewski, <strong>2000</strong>a). A paper containing these results<br />

has been submitted (Vanelle and Gajewski, <strong>2000</strong>c).<br />

APPENDIX A<br />

The weight function in equation (4) contains the Hessian matrix of the difference between<br />

diffraction (»¨¼ ) and reflection (»x ) traveltimes. To write !€ in terms of second<br />

derivatives of traveltimes we will now derive expressions »¼ for »¨x and containing<br />

first and second derivatives. Consider an arbitrary velocity model. Let sources be<br />

positioned in a reference surface that we will denote the source surface. If the resulting<br />

traveltime field for a source at the Š position<br />

½ ¾<br />

is single-valued, the traveltime<br />

from a<br />

½<br />

point in the source surface and in a near<br />

½ ¾ ½ª¿À“<br />

vicinity of to a subsur-<br />

Š<br />

½ ½ ¿¾<br />

Š<br />

near can be expressed by a Taylor series Á ½Â• ½Äà ½ ¿ ¾<br />

provided that<br />

• ½ ¿ Ã ½ ¿¾<br />

Š<br />

Š<br />

are small, the size of this small vicinity depends on the<br />

¿<br />

model<br />

½<br />

face Š point<br />

Á Š and<br />

under consideration and the required accuracy. For a multi-valued traveltime field the<br />

Taylor expansion is valid if the different branches of the traveltime curve are treated<br />

separately. Š As<br />

» Š<br />

½ ‘<br />

½ ¾<br />

lie in one surface the traveltimes are expanded into the surface<br />

traveltime expansion looks as follows:<br />

½Å¿¾ if Š<br />

and<br />

½<br />

Š<br />

in this variable. We also » expand into a surface Š in<br />

½Å¿<br />

, this will be the reflector surface,<br />

or, more precisely, the reflector's tangent plane at Š<br />

½ª¿<br />

is on a curved reflector. The<br />

Æ Á ¿ ¿ ÃÈÇ É Á ½ ¨ ½ ¦ Ê<br />

Á ½<br />

Š<br />

«<br />

Š Š Š<br />

ÉÇ<br />

¿ ¦ ¨ ½ ¿ ½ Ã Ë ½ ¨ ¦ §<br />

Š Á Á Š Á Š<br />

(A-1)<br />

» ¾–Ã<br />

» Š<br />

½ ‘<br />

Š<br />

½ ¿ “–•<br />

Æ ½<br />

Š<br />

« Á Š<br />

Á Š<br />

½ ¿<br />

where the first order traveltime derivatives<br />

%Ô ‘Õ •<br />

‘ É “<br />

(A-2)<br />

ÐOÑÒ<br />

Ð#ÓÑ<br />

ÐOÑNÒ<br />

Ð#ÓÑ

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