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S-Cube is at Transforming Energy Exploration in Bengaluru, India, Sep 23–25!

Subsurface clarity, redefined.

Time Space Lag FWI is S-Cube's next-generation Full Waveform Inversion — clearer and deeper seismic imaging, with smarter, faster AI-driven decision making built into the platform.

Land & marine2D & 3DAcoustic & elasticCloud native

Collaborating with Global Leaders in Energy and Technology

  • Chevron
  • EPAM
  • AWS
  • Petrobras
  • Imperial College London
  • Aspentech
  • Shell Logo
  • Google Cloud Platform
  • ONGC
  • Woodside Energy
  • Azure
Fixing a broken model

Latest prospects

Each project targets a different challenge — a snow zone, prospect depth, a new frontier. Step through the model evolution and see how targeted FWI resolves it.

01

West Harrison Bay

North Slope Alaska · USA

Challenge · Ungrounded-ice snow zone

Identifying prospective amplitude anomalies under a layer of severe permafrost

2 BN bbl
Oil reserves estimated
5
Prospects defined
45 Hz
TSL-FWI, 2 surveys merged
Open the case page
Inline 306: the legacy tomographic velocity model over the KPSDM migrated with it, nothing resolved in the snow zone
Inline 306: the 16 Hz macro TSL-FWI velocity model, broad structure returning and horizons flattening below the unconformity
Inline 306: the 45 Hz macro TSL-FWI velocity model, the snow zone opening up and clinoforms beginning to show
Inline 306: the 45 Hz targeted TSL-FWI velocity model, clinoforms resolved in the migration and in the velocity model itself
1 / 4Legacy model

Inline 306 — TSL-FWI velocity over the KPSDM migrated with that model, from the legacy model through to the 45 Hz targeted update.

02

Highlander 3

South Louisiana · USA

Challenge · Depth of prospect

Imaging a 30kft deep target with only 20k offsets

30 kft
Austin Chalk target depth
20 kft
Maximum offset
1.6 TCF
Estimated
Open the case page
Inline 177 and crossline 323 Vp — the starting velocity model, a smooth layer-cake gradient to 9.5 km
Inline 177 and crossline 323 Vp after the sub-salt macro update from reflection waveform inversion
Inline 177 and crossline 323 Vp after the final high-resolution TSL-FWI pass, resolving stratigraphy at 8.5 to 9 km
1 / 3Starting model

Inline 177 and crossline 323 Vp — from the starting model to the prospect-defining TSL-FWI result.

03

Mahanadi Basin

Mahanadi Basin · India

Challenge · New exploration frontier

Defining prospective channels from scratch

450–1,500 m
Water depth
2026
First drilled
$12 BN
Deepwater exploration campaign
Read the case study
Mahanadi Basin 1750 m depth slice — starting model
Mahanadi Basin 1750 m depth slice — inverted model revealing gas-charged channels
1 / 2Starting model

1750 m depth slice — low-velocity anomalies in the Mio–Pliocene CLCs reveal proven gas-charged channels.

Showcase

What TSL-FWI can do

Three projects where the story is the method rather than the prospect — a target moved 650 ft and proved blind at the well, a model built from no starting model at all, and elastic salt that acoustic inversion cannot recover.

04

Highlander 2

South Louisiana · USA

Challenge · Blind tie · 650 ft

Extracting a velocity update to fix a 650ft pull up between two wells 2 miles apart

650 ft
Target shift, matched at the well
2 miles
From Highlander 1 to the blind tie
150 ft
Net pay
Open the case page
RTM through the Austin Chalk interval on the starting model — at Highlander 2 the chalk sits 650 ft above where the well found it, and the reflectors break up between the wells
The same interval on the final TSL-FWI model — an event arrives at the pick at both wells, continuous across the gap, with the 650 ft move down at Highlander 2 marked
1 / 2Starting model

Austin Chalk target interval, 26–30 kft — RTM on the starting model and on the final TSL-FWI model, with the 650 ft move down at Highlander 2 marked.

05

Alaminos Canyon

Gulf of Mexico · USA

Challenge · No starting model · sub-salt

Mapping a 6km deep target layer under a complex salt structure built from scratch

2,000 m/s
Initial error at the blind log
6 km
Target depth, sub-salt
No wells
Nothing well-derived in the inversion
Follow the live build
Alaminos Canyon crossline 414 — M0, a regional compaction trend with no structure and no salt
Alaminos Canyon crossline 414 — T2, salt geometry and the sediment section recovered, continuity still lost under the salt
Alaminos Canyon crossline 414 — T3, continuity restored under the salt and deep compacted sediment resolved
1 / 3M0 · Starting model

Crossline 414 Vp — M0's compaction trend through T2 to T3, with continuity restored under the salt.

06

Tupi

Santos Basin · Brazil

Challenge · Elastic salt · layered anhydrites

Recovering sub-salt targets from a featureless compaction trend

Multiparameter
Elastic AWI + RWI
Sub-salt targets
Recovered under layered anhydrites
20 Hz
Elastic FWI
Read the case study
Santos Basin start Vp on a cross-line in the sub-salt dip direction — a featureless compaction trend under the water layer
The same cross-line after acoustic FWI to 5 Hz, the salt body taking shape but the section still blocky
The same cross-line after elastic FWI to 20 Hz, top salt sharply resolved and the sub-salt section recovered
1 / 3Start Vp

Vp on a cross-line in the sub-salt dip direction — start model through 5 Hz acoustic to 20 Hz elastic FWI.

The enabler · XWAI

What makes these workflows possible

Behind every defined prospect is XWAI — S-Cube's AI copilot built into the X-Wave platform. It drives the advanced inversion workflows that turn difficult data into superior results.

Targeted, not brute-force

XWAI sequences AWI, RWI and FWI to the exact problem in each dataset — so the model converges on the prospect, not the noise.

Faster to a defined model

Automated QC and parameter selection cut the iterations between an early model and a drillable result from weeks to days.

Everyone can interrogate it

Sequences, jobs, parameters and cost — and rendered velocity slices — all answered in plain language, grounded in live project data.

Global Impact

Transforming seismic imaging across the world's most challenging basins

Further project locations: Permian Basin, South Louisiana, Bengal Basin, India, Uzbekistan Onshore, Green Canyon, Gulf of America, Garden Banks, Gulf of America, Offshore Malaysia — Petronas, Magnus, North Sea UK, Scarborough, Australia, Bonaparte Basin, Australia, North West Shelf, Australia

Ready to see your data in high definition?

Let's discuss how S-Cube XWI can transform your seismic projects — schedule a private demonstration with our imaging experts, or jump straight into XWAI.

info@s-cube.com