%0 Journal Article %1 buske:1999a %A Buske, S. %D 1999 %J Pure and Applied Geophysics %K geophysics seismics %N 1-2 %P 157--171 %R 10.1007/s000240050294 %T 3-D prestack Kirchhoff migration of the ISO89-3D data set %U http://dx.doi.org/10.1007/s000240050294 %V 156 %X This paper presents an overview of the results obtained from a 3-D prestack depth migration of the ISO89-3D data set. The algorithm is implemented as a Kirchhoff-type migration, in which the migrated image is generated by weighted summation along diffraction surfaces through the shot record section. The diffraction surfaces are computed by a 3-D finite difference solution of the eikonal equation. A 3-D macro-velocity model derived mainly from wide-angle tomographic inversion served as input for the travel-time calculations. The results of the migration are presented as slices through a volume covering an area of 21 km 2 21 km in the horizontal and 15 km in the vertical direction, centered around the KTB drill hole. In these slices the continuation of the Franconian Lineament or SE1 reflector, respectively, can be identified over most of the survey area as a northeast dipping reflector plane. Its signature appears partly curved and discontinuous and with different strength of reflection down to a maximum depth of 9 km. About 5 km to the south-southeast of the KTB drill hole the uppermost top reflection of the Erbendorf body (EB) can be recognized at approximately the same depth. The slices clearly show its complicated internal structure consisting of several apparently separated reflective parts. Moreover, the geometry and the shape of a few other subsurface structures are described.

@article{buske:1999a, abstract = {This paper presents an overview of the results obtained from a 3-D prestack depth migration of the ISO89-3D data set. The algorithm is implemented as a Kirchhoff-type migration, in which the migrated image is generated by weighted summation along diffraction surfaces through the shot record section. The diffraction surfaces are computed by a 3-D finite difference solution of the eikonal equation. A 3-D macro-velocity model derived mainly from wide-angle tomographic inversion served as input for the travel-time calculations. The results of the migration are presented as slices through a volume covering an area of 21 km 2 21 km in the horizontal and 15 km in the vertical direction, centered around the KTB drill hole. In these slices the continuation of the Franconian Lineament or SE1 reflector, respectively, can be identified over most of the survey area as a northeast dipping reflector plane. Its signature appears partly curved and discontinuous and with different strength of reflection down to a maximum depth of 9 km. About 5 km to the south-southeast of the KTB drill hole the uppermost top reflection of the Erbendorf body (EB) can be recognized at approximately the same depth. The slices clearly show its complicated internal structure consisting of several apparently separated reflective parts. Moreover, the geometry and the shape of a few other subsurface structures are described.}, added-at = {2012-09-01T13:08:21.000+0200}, author = {Buske, S.}, biburl = {https://www.bibsonomy.org/bibtex/2de6c77e476f60fea7035ae60c11c794f/nilsma}, day = 1, doi = {10.1007/s000240050294}, interhash = {1bda6a03c43a0488143bb40d228e9274}, intrahash = {de6c77e476f60fea7035ae60c11c794f}, journal = {Pure and Applied Geophysics}, keywords = {geophysics seismics}, month = sep, number = {1-2}, pages = {157--171}, timestamp = {2021-02-09T13:27:42.000+0100}, title = {3-D prestack Kirchhoff migration of the ISO89-3D data set}, url = {http://dx.doi.org/10.1007/s000240050294}, volume = 156, year = 1999 }