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pro vyhledávání: '"Richard Ottolini"'
Autor:
Richard Ottolini, Jon F. Claerbout
Publikováno v:
GEOPHYSICS. 49:237-249
Reflection seismic data can be imaged by migrating common midpoint slant stacks. The basic method is to assemble slant stack sections from the slant stack of each common midpoint gather at the same ray parameter. Earlier investigators have described
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ecae7cc90a4cb8a647b1930e490297eb
https://doi.org/10.1190/1.1441656
https://doi.org/10.1190/1.1441656
Autor:
George A. McMechan, Richard Ottolini
Publikováno v:
Bulletin of the Seismological Society of America. 70:775-789
The well known Wiechert-Herglotz technique for computing a velocity-depth profile from refraction seismograms uses data in the form of ray parameter as a function of intercept time (a p-τ curve). The technique of slant stacking used by reflection se
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4d1d736c5eb9845af33f609420358804
https://doi.org/10.1785/bssa0700030775
https://doi.org/10.1785/bssa0700030775
Publikováno v:
GEOPHYSICS. 49:195-200
On‐line movies are an exciting way to view reflection seismic data. We make a movie by slicing through a three‐dimensional (3-D) seismic data cube in a selected direction (Figure 1). By sweeping through the data fast enough, it is possible to get
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5b86bc16e5ae85bb42890adc7590557d
https://doi.org/10.1190/1.1441652
https://doi.org/10.1190/1.1441652
Publikováno v:
SEG Technical Program Expanded Abstracts 1984.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::290006ca1744af527713773fc9257551
https://doi.org/10.1190/1.1894213
https://doi.org/10.1190/1.1894213