Model-Based Interpretation of Time-Lapse Seismic, Using Stochastic Matching

Author(s):  
D. Gawith Ltd. ◽  
P. Gutteridge
2018 ◽  
Vol 38 (1) ◽  
pp. 194-209
Author(s):  
Paul J. Askey ◽  
Hillary Ward ◽  
Theresa Godin ◽  
Marcus Boucher ◽  
Sara Northrup

2014 ◽  
Vol 15 (3) ◽  
pp. 156-160 ◽  
Author(s):  
Ender Yalcinkaya ◽  
Elif G. Ergin ◽  
Eray Caliskan ◽  
Zeynep Oztel ◽  
Alev Ozay ◽  
...  

2015 ◽  
Vol 16 (1) ◽  
pp. 29
Author(s):  
Suhayat Minardi ◽  
Teguh Ardianto

The research has a goal to develop a model-based filter to separate the time lapse microgravity anomali caused by the 3 pieces of the source of anomalies with different depths. The activities which included in this research are: geological modeling, calculation of time lapse microgravity responses caused by several sources, designing of digital model based filter, application of the filter to separate synthetic time lapse microgravity anomali data, and performance test of the filter. Designed model is multi aquifer sistem with homogeny isotropic properties at different depth. Equipment of this research is a unit computer with MATLAB Version 7.11.0.584 (R2010b) and Microsoft Excel 2007 software. The designed filter can separate time lapse microgravity anomali based on its sources successfully with error less than 5%.Keywords: Filter, synthetic, time lapse microgravity anomaly 


2018 ◽  
Vol 37 (12) ◽  
pp. 2630-2641 ◽  
Author(s):  
Dmitry V. Sorokin ◽  
Igor Peterlik ◽  
Vladimir Ulman ◽  
David Svoboda ◽  
Tereza Necasova ◽  
...  
Keyword(s):  

Geophysics ◽  
2018 ◽  
Vol 83 (4) ◽  
pp. Q25-Q35 ◽  
Author(s):  
Yang Zhao ◽  
Weichang Li

Interferometric virtual source (VS) redatuming converts surface-triggered source records into the equivalent records as if they originated from buried receiver locations by crosscorrelating downgoing waves with the corresponding upgoing waves. The theory suggests that when the receivers are surrounded by an enclosing boundary of sources, then the VS has an isotropic radiation pattern and yields an accurate response. The resultant records should determine improvement in the seismic repeatability and image quality compared with non-VS. However, in the presence of a complex near surface, an intricate shallow structure and highly variable weathering layers can severely distort the raypath, such that it produces uneven angle coverage to the buried VS. In addition, near-surface reverberations, surface multiples, and other mode-converted waves may leak into the time-gated early arrivals and further corrupt the direct wavefields. The above-mentioned issues can result in distorted radiation patterns and contaminated responses of the VS. We address these issues explicitly by spatially filtering the potentially contaminated direct wavefields using a zero-phase matched filter, such that the filtered wavefield is consistent with a model-based ideal direct P-wavefield observed at common receiver locations. This ideal reference response is computed from a homogeneous approximation to the local near-surface overburden on top of each VS. The phases of the original direct arrivals are preserved. Components associated with the reverberations and other noises can be effectively suppressed as their spatial radiation patterns deviate from that of the ideal single P-wave mode. Toward an isotropic radiation pattern by the iterative matched filter, we reduce the unbalanced illumination arising from imperfect source coverage and near-surface complexity. Compared with previous methods, the new VS approach provides significantly improved image quality and repeatability based on a pilot field of 13 time-lapse surveys, which solved a significant repeatability problem across a 17 month survey gap.


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