System and method for seismic amplitude analysis
US-2024125956-A1 · Apr 18, 2024 · US
US9229121B2 · US · B2
| Field | Value |
|---|---|
| Publication number | US-9229121-B2 |
| Application number | US-201313795072-A |
| Country | US |
| Kind code | B2 |
| Filing date | Mar 12, 2013 |
| Priority date | Mar 13, 2012 |
| Publication date | Jan 5, 2016 |
| Grant date | Jan 5, 2016 |
A practical reading order for non-experts. Skip the full description unless you need deep technical detail.
What the patent document calls the invention.
A short plain-language summary of the technical disclosure.
Who owns or filed the patent and who is credited as inventor.
Filing, priority, publication, and grant dates set the timeline.
The legal scope of protection — read this for what is actually claimed.
Technology tags used to group this patent with similar filings.
Prior art links and similar publications in this corpus.
Official abstract text for this publication.
The description relates to a seismic imaging technology technique for modeling a subsurface structure through waveform inversion in the Laplace domain. The seismic imaging system comprises a scaled gradient calculating unit calculating a scaled gradient, a modeling parameter updating unit updating the model parameters using the scaled gradient direction, and an iteration control unit controlling the scaled gradient calculating unit and the modeling parameter updating unit to repeat processing iteratively until a stopping criteria is met.
Opening claim text (preview).
What is claimed is: 1. A seismic imaging system using Laplace-domain wave equation in acoustic-elastic coupled media, comprising: a scaled gradient calculating hardware circuit calculating a scaled gradient direction of an objective function by multiplying a gradient of the objective function and an accumulated gradient, wherein the accumulated gradient is calculated using a vertically accumulated square sum of original gradient values by summing an accumulated gradient of a previous vertical layer and a square of the gradient of the objective function, and the objective function is defined by a residual of logarithmic wavefield in Laplace domain; a modeling parameter updating hardware circuit updating model parameters for a discretized finite element equation for the acoustic-elastic coupled media from a Laplace-transformed acoustic wave equation, a Laplace-transformed elastic wave equation and continuity conditions at an interface between an acoustic media and an elastic media of the acoustic-elastic coupled media; an iteration control hardware circuit controlling the scaled gradient calculating circuit and the modeling parameter updating hardware circuit to repeat processing iteratively until a stopping criteria is met; and an imaging hardware circuit converting Lamè constants into P-wave velocity, S-wave velocity, and density and generating a submarine subsurface image showing the distribution of P-wave and S-wave velocities. 2. The seismic imaging system in claim 1 , wherein the system further comprises a source wavelet estimation hardware circuit estimating an unknown source wavelet from an initial source using a full Newton method and outputting the result to the modeling parameter updating hardware circuit. 3. The seismic imaging system of claim 1 , wherein the accumulated gradient is always positive. 4. A seismic imaging method using Laplace-domain wave equation in acoustic-elastic coupled media, comprising: calculating, using a scaled gradient calculation hardware circuit, a scaled gradient direction of an objective function by multiplying a gradient of the objective function and an accumulated gradient, the accumulated gradient being calculated using a vertically accumulated square sum of original gradient values by summing an accumulated gradient of a previous vertical layer and a square of the gradient of the objective function, wherein the objective function is defined by a residual of logarithmic wavefield in Laplace domain; updating model parameters for a discretized finite element equation for the acoustic-elastic coupled media from a Laplace-transformed acoustic wave equation, a Laplace-transformed elastic wave equation and continuity conditions at an interface between an acoustic media and an elastic media of the acoustic-elastic coupled media; repeating calculating the scaled gradient direction and updating the model parameters iteratively until a stopping criteria is met; and converting, using an imaging hardware circuit, Lamè constants into P-wave velocity, S-wave velocity, and density and generating a submarine subsurface image showing the distribution of P-wave and S-wave velocities. 5. The seismic imaging method in claim 4 , wherein updating the model parameters includes estimating an unknown source wavelet from an initial source using a full Newton method.
Application of seismic models, synthetic seismograms · CPC title
Related publications grouped by family.
Answers are generated from the same data shown on this page.