Second EAGE/PESGB Workshop on Velocities 2019
DOI: 10.3997/2214-4609.201900051
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Salt Stratification and Least Square Migration to Improve Pre-Salt Reservoir Images: Santos Basin, Brazilian Offshore Example

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Cited by 4 publications
(5 citation statements)
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“…We can also note that when we add the detailed velocity model (with the stratification insertion) the results are even better. This last statement confirms that least-squares schemes in the velocity models associated with detailed velocity models has potential to deliver more accurate amplitude responses for the pre-salt targets in the Santos Basin, as pointed in some previous works (Ji et al, 2011;Wang et al, 2017;Fonseca et al, 2018;Dias et al, 2019;Shadrina et al, 2020).…”
Section: Figure 3 -Frequency Content Of the Five Built Images Includi...supporting
confidence: 87%
“…We can also note that when we add the detailed velocity model (with the stratification insertion) the results are even better. This last statement confirms that least-squares schemes in the velocity models associated with detailed velocity models has potential to deliver more accurate amplitude responses for the pre-salt targets in the Santos Basin, as pointed in some previous works (Ji et al, 2011;Wang et al, 2017;Fonseca et al, 2018;Dias et al, 2019;Shadrina et al, 2020).…”
Section: Figure 3 -Frequency Content Of the Five Built Images Includi...supporting
confidence: 87%
“…The methodology presented in this work results in an improved initial velocity model for seismic tomography, lowering the computational efforts when compared to the conventional approach ("salt flooding" + inversion tomographic updates), as cited by ), Falcão (2017), Maul et al (2018a), Dias et al (2019 and Maul et al (2019).…”
Section: Discussionmentioning
confidence: 99%
“…These groups are: (i) the Low Velocity Salts/Evaporites group (LVS), mainly composed by carnallite, tachyhydrite, sylvite and other mobile salts; which present compressional velocities lower than the represented by the halite mineral (4,500 m/s); (ii) the Halite group, usually abundant and considered as the background group; represented by the compressional velocity of about 4,500 m/s; and (iii) the High Velocity Salts/Evaporites group (HVS), basically composed by anhydrite and gypsum, having compressional velocities higher than 4,500 m/s. Intrusive rocks, when found, due to the same velocity behavior as HVS minerals, were also considered inside this group -an approach that has been adopted in many case studies (Meneguim et al, 2015;González et al, 2016;Falcão et al, 2016;Barros et al, 2017;Fonseca et al, 2017Fonseca et al, , 2018Teixeira et al, 2018;Maul et al, 2018aMaul et al, ,b, 2019Dias et al, 2019). Fonseca et al (2017) also observed carbonate and siliciclastic occurrences within the salt section, and suggested to group them within the Halite group, as their velocity behaviors are more similar to this background's group.…”
Section: Introductionmentioning
confidence: 99%
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“…During the methodology development, several applications have taken advantage of using this strategy of modeling evaporitic stratifications. The more promising applications are related to uncertainties Jardim et al, 2015), geomechanics (Toríbio et al, 2017;Teixeira et al, 2018), Kirchhoff migration and Reverse Time Migration -RTM (Gobatto et al, 2016;Fonseca et al, 2018;Maul et al, 2018a) and the initial model for Least-Square Migration (Dias et al, 2019).…”
Section: Introductionmentioning
confidence: 99%