Zobrazeno 1 - 10
of 35
pro vyhledávání: '"H F, Gardner"'
Autor:
Anat Canning, Gerald H. F. Gardner
Publikováno v:
GEOPHYSICS. 63:1177-1183
The acquisition patterns of 3-D surveys often have a significant effect on the results of dip moveout (DMO) or prestack migration. When the spatial distribution of input traces is irregular, results from DMO and migration are contaminated by artifact
Autor:
Gerald H. F. Gardner, Anat Canning
Publikováno v:
GEOPHYSICS. 63:686-691
A common midpoint (CMP) gather usually provides amplitude variation with offset (AVO) information by displaying the reflectivity as the peak amplitude of symmetrical deconvolved wavelets. This puts a reflection coefficient R at every offset h, giving
Autor:
Gerald H. F. Gardner, Anat Canning
Publikováno v:
GEOPHYSICS. 61:1103-1114
The combination of DMO and [Formula: see text] is used here to change the original acquisition geometry of a 3-D seismic data set into a more convenient form. For example, irregular 3-D surveys can be projected onto a regular midpoint‐offset grid w
Autor:
Gerald H. F. Gardner, Anat Canning
Publikováno v:
GEOPHYSICS. 61:409-421
A two‐pass approximation to 3-D Kirchhoff migration simplifies the migration procedure by reducing it to a succession of 2-D operations. This approach has proven very successful in the zero‐offset case. A two‐pass approximation to 3-D migration
Publikováno v:
GEOPHYSICS. 56:2036-2047
A thin sand has been successfully imaged at great depth using a carefully designed, high‐resolution, three‐dimensional (3-D), seismic survey. The area of the survey was along a portion of the boundary between northeastern Vermilion Parish and sou
Publikováno v:
Geophysical Research Letters. 18:1389-1392
The Fourier spectral centroid formula for instantaneous frequency is extended to all times and to all analytic signals and is in a convenient computable form. Examples using two different synthetic even seismic wavelets show that the peaks and trough
Autor:
James L. Black, Matthew A. Brzostowski, Biondo Biondi, Sergey B. Fomel, Nizar Chemingui, Anat Canning, Gerald H. F. Gardner, N. L. Mohan, John Etgen, Carl Regone, Ian F. Jones, Juergen K. Fruehn, Sheng Xu, Yu Zhang, Don Pham, Gilles Lambaré
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fc1560c1e8d18ca205e1b6314bb010ba
https://doi.org/10.1190/1.9781560801917.ch2
https://doi.org/10.1190/1.9781560801917.ch2
Publikováno v:
GEOPHYSICS. 55:863-867
When a common‐midpoint gather is collected above a dipping reflector, the point at which reflection occurs moves updip as the source‐receiver offset increases. Stacking velocity is constant, but it is a function of dip. Hence a stacked trace is n
Publikováno v:
SEG Technical Program Expanded Abstracts 1996.
Publikováno v:
SEG Technical Program Expanded Abstracts 1996.