2021
DOI: 10.1093/gji/ggab388
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A joint inversion-segmentation approach to assisted seismic interpretation

Abstract: Summary Structural seismic interpretation and quantitative characterization are historically intertwined processes. The latter provides estimates of the properties of the subsurface, which can be used to aid structural interpretation alongside the original seismic data and a number of other seismic attributes. In this work, we redefine this process as an inverse problem which tries to jointly estimate subsurface properties (i.e., acoustic impedance) and a piece-wise segmented representation of t… Show more

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Cited by 13 publications
(8 citation statements)
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References 36 publications
(39 reference statements)
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“…Note that the right‐hand‐side of Equation can be interpreted as a series of post‐stack seismic inversions (one post‐stack inversion per petrophysical parameter), which are solved here using the PyLops computational framework (Ravasi & Vasconcelos, 2020). Moreover, whilst we have considered a single location for simplicity in this derivation, the final step of inversion is usually carried out for all spatial locations at the same time, such that spatial regularization in the form of Laplacian or Total Variation (e.g., Ravasi & Birnie, 2022) can be introduced.…”
Section: The Seis2rock Methodsmentioning
confidence: 99%
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“…Note that the right‐hand‐side of Equation can be interpreted as a series of post‐stack seismic inversions (one post‐stack inversion per petrophysical parameter), which are solved here using the PyLops computational framework (Ravasi & Vasconcelos, 2020). Moreover, whilst we have considered a single location for simplicity in this derivation, the final step of inversion is usually carried out for all spatial locations at the same time, such that spatial regularization in the form of Laplacian or Total Variation (e.g., Ravasi & Birnie, 2022) can be introduced.…”
Section: The Seis2rock Methodsmentioning
confidence: 99%
“…Finally, an inverse problem is solved to undo the effect of the wavelet W and time-derivative T operators: where R is the matrix containing the petrophysical reflectivities from the well log used in training of size n ⋅ N t × n m , and H p = V T p Λ 1 p is a matrix of size N t × p. Note that the right-hand-side of Equation 5 can be interpreted as a series of post-stack seismic inversions (one post-stack inversion per petrophysical parameter), which are solved here using the PyLops computational framework (Ravasi & Vasconcelos, 2020). Moreover, whilst we have considered a single location for simplicity in this derivation, the final step of inversion is usually carried out for all spatial locations at the same time, such that spatial regularization in the form of Laplacian or Total Variation (e.g., Ravasi & Birnie, 2022) can be introduced.…”
Section: Inference Stagementioning
confidence: 99%
“…In this paper, we propose the use of the JIS algorithm [9,7,10], which in addition to TV regularization terms, it incorporates a segmentation constraint over the estimated 4D difference. As such, 4D JIS not only retrieves highresolution baseline and monitor acoustic impedance models, but also segments the monitor-baseline acoustic impedance difference into multiple probability volumes based on user-defined time-lapse classes.…”
Section: Regularizationmentioning
confidence: 99%
“…Equation 4presents a non-convex optimization problem that becomes convex when fixing one of the optimization variables ( m, V ). Therefore its solution is found in an alternating fashion, where each variable is optimized independently at every iteration using the Primal-Dual algorithm [11]; for more implementation details, we refer the reader to [9].…”
Section: Regularizationmentioning
confidence: 99%
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