High-fidelity seismic modeling and imaging for complex geology.

3Dcomplex geology
More than one trillionunknowns demonstrated
Cloud + HPCone simulation model

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Seismic Modeling Reimagined

Finite Element Method

  • Flexible: Complex geometries
  • Accurate: High-order geometry and fields
Three-dimensional high-order finite-element mesh

Adaptive Meshing

  • Optimal: Concentrates effort where needed
  • Automated: No tedious mesh tuning
Adaptive finite-element mesh concentrated around complex geometry

Fast Frequency-Domain Solver

  • Stable: No CFL condition
  • Scalable: More than one trillion 3D unknowns demonstrated
High-resolution simulated seismic wavefield

Frequency Domain vs. Time Domain

FrequenSolve enables unparalleled frequency-domain simulation, often >100x faster than leading time-domain tools.

Time-domain simulation is also supported by combining frequencies. This can often be competitive with leading time-domain finite difference codes and is especially competitive in cases with:

  • Attenuation
  • Anisotropy
  • High contrast
  • Topography / complex geometry
Frequency-domain Scholte-wave simulation

Frequency-Domain

Time-Domain

How it Works

1

FrequenSolve's intuitive Python interface combines models, acquisition geometries, and data into 'simulations'.

2

Simulations can be run at various 'sites' where our fast solver code is installed and licensed, including:

  • AWS cloud via FrequenSol's API
  • On-prem HPC clusters
3

Simulations can be run in forward, adjoint, and gradient mode, in both frequency- and time-domain.

4

Results are stored on the cloud or HPC site, FrequenSolve provides secureand convenient methods for retrieving, exporting, and plotting results.

5

FrequenSolve defines customizable imaging workflows including Reverse Time Migration (RTM) and Full-Waveform Inversion (FWI), or can be used as a modeling backend for proprietary imaging algorithms.

FrequenSolve Python client simulation example

Use Cases

3D Topography Modeling

Model high-precision surface topography directly instead of relying on extensive static corrections.

Explore 3D Topography Modeling

Flat topography

Dune topography

Scholte Wave Modeling

Resolve slow Scholte waves across fluid-sediment interfaces with localized adaptive meshes.

Explore Scholte Wave Modeling
Adaptive finite-element mesh aligned to a fluid-sediment interface

Adaptive interface mesh

Synthetic Scholte-wave seismic gather

Modeled Scholte-wave data

Seismic Speckle Modeling

Capture scattering from fine-scale heterogeneity in slow, weathered near-surface layers.

Explore Seismic Speckle Modeling
Near-surface seismic velocity model containing fine-scale heterogeneity

Heterogeneous near-surface model

Synthetic seismic gather showing near-surface speckle scattering

Modeled scattered wavefield

3D Borehole and Fracture Modeling

Represent boreholes and fractures directly to resolve tube and Krauklis-wave behavior in 3D.

Explore 3D Borehole and Fracture Modeling
Three-dimensional finite-element mesh surrounding a fluid-filled borehole

3D borehole finite-element mesh

Features

Domain
  • Frequency
  • Time
Dimensions
  • 2D
  • 3D
Physics
  • Acoustic
  • Elastic
  • Electromagnetic
  • Coupled Multi-physics
Modes
  • Forward
  • Adjoint
  • Gradient
Interface
  • Python Client
Platform
  • Cloud
  • HPC

Choose how to run FrequenSolve

Start with a free Cloud trial or explore an On-Prem and Hybrid HPC deployment.