A · Advanced seismic imaging and scientific computing
Entry: the solver is validated on synthetic cases (P2), then each method is compared with its baseline.
Research
What we will test, how we will judge it, and what we will refuse to claim.
Eight phases, P0 to P7. Each closes with a test, not a date.
Programs A, B and C advance alongside the phases, each behind its own entry criterion.
Entry: the solver is validated on synthetic cases (P2), then each method is compared with its baseline.
Entry: seismic baselines exist (P3), then each extra data type is tested for added information (P5).
Entry: a written feasibility and marine-limits review for each concept; nothing is built until a concept passes it.
How any result will be judged before it is shown.
Every method is compared with a baseline on the same data, with the same inputs and the same compute budget.
Test data are separated from training and tuning data by survey and by geology, not by random split.
We reject images without quantitative truth metrics.
Every claim on the site, with the evidence behind it. A claim appears here only once evidence exists.
The ledger is empty on purpose. It fills as results are validated and reviewed, and until then every claim on the site stays at concept.
What this program cannot do, and what remains to be shown.
Better images can inform decisions. They do not create resources or promise that any is present.
The deeper the target, the coarser the detail the data can support.
Different models can fit the same data, which is why we report ranges, not single answers.
Real data belong to their owners. We work on synthetic and open data until a partner is licensed to share more.
That is why learned components are tested against held-out geology and cannot certify results.
Only direct sampling confirms what is in the ground.
A sensor or method that works in shallow water must still be shown to work in deep water.
No publications yet. Papers, datasets and code will be listed here when they are released.