The Impact of Reverse Time Migration on the Evaluation of Mature Southern North Sea Assets

Author(s):  
S. Fletcher

2021 ◽  
Author(s):  
Hala Alqatari ◽  
Thierry-Laurent Tonellot ◽  
Mohammed Mubarak

Abstract This work presents a full waveform sonic (FWS) dataset processing to generate high-resolution images of the near-borehole area. The dataset was acquired in a nearly horizontal well over a distance of 5400 feet. Multiple formation boundaries can be identified on the final image and tracked at up to 200 feet deep, along the wellbore's trajectory. We first present a new preprocessing sequence to prepare the sonic data for imaging. This sequence leverages denoising algorithms used in conventional surface seismic data processing to remove unwanted components of the recorded data that could harm the imaging results. We then apply a reverse time migration algorithm to the data at different processing stages to assess the impact of the main processing steps on the final image.





Author(s):  
I. F. Jones ◽  
M. J. Sugrue ◽  
D. G. King ◽  
M. C. Goodwin ◽  
I. D. Berranger ◽  
...  


2007 ◽  
Author(s):  
I. F. Jones ◽  
M. C. Goodwin ◽  
I. D. Berranger ◽  
H. Zhou ◽  
P. A. Farmer




2014 ◽  
Vol 33 (9) ◽  
pp. 986-992 ◽  
Author(s):  
Andrew Ratcliffe ◽  
Antonio Privitera ◽  
Graham Conroy ◽  
Vetle Vinje ◽  
Alexandre Bertrand ◽  
...  


Geophysics ◽  
2011 ◽  
Vol 76 (2) ◽  
pp. B33-B42 ◽  
Author(s):  
Alison E. Malcolm ◽  
Maarten V. De Hoop ◽  
Bjørn Ursin

As more resources are directed toward reverse time migration, an accurate velocity model, including strong reflectors, is necessary to form a clear image of the subsurface. This is of particular importance in the vicinity of salt, where singly scattered waves are often not ideal for imaging the salt flanks. This has led to interest in processing doubly scattered waves (also called duplex or prismatic waves) for imaging salt flanks and thus improving the location of salt boundaries in a velocity model. We used doubly scattered waves in a two-pass, one-way method to image salt flanks in a North Sea data set. By working in the one-way framework we were able to separately construct images with singly, doubly, and triply scattered waves. We used a multistep imaging process that includes multiply scattered waves by using an imaged reflector to fix one (or more) of the scattering points, allowing for multiply scattered energy from several reflectors, potentially with poor continuity, to be included without picking each reflector individually. With this method we were able to image the flank of a North Sea salt body.



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