Our Features
Molecular-level simulation adhering to the geophysical theoretics violated by existing software
Easy-to-use computational physics, even for non-experts



Accuracy
Our system models matter down to its subatomic structure to create physical simulations with reliable atomic-level influences.
Multistate
Porous granular material and rock-mass fractures filled with varying mixed-state compositions as well as melting near the earth's core.
Multiphysics
Simultaneous mechanical and electromagnetic perturbations including their coupling within matter.
Multiscale
Continuum mechanics augmented with nano-scale details such as defect induced plasticity and features of elastic attenuation, dispersion, and interfacing that are not accounted for with large scale approximations.
Non-Equilibrium
Porous flow of matter into and within the system and heat flow from underground thermal sources.
Relativity
Location dependent gravitational field and heavy element effects.
Irregular Sources
Mechanical loading by non-planar irregularly shaped indentations and at rates over the speed of elastic dissipation.
Data augmentations for machine learning model functionality
Train models that automatically and robustly ignore signal influences without subsurface insight
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Encoding
Efficient methods of encoding multi-dimensional physical signals and subsurface models to create reduced representations without loss of information.​

Sensor Effects
Augment data with the effects of measurement digitalization and randomized sensor-system coupling. Create a model insensitive to the device used for measurement.
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Noise
Include randomized realistic noise that covers the spectrum of signal interference seen in the real world. Models will learn to ignore these additions during optimization.
Realistic subatomic geology models subject to user provided customization
Simulate data from randomly generated structures obeying statistical variations in geology

Lithostratigraphy
Our models feature realistic changes in lithology based on geologic time and location, including plausible geochemical variations within and among the lithologic units.
Geographic considerations
Diverse marine and terrestrial environments
Mineral Crystallization
We simulate mineral crystallization according to real-rock grain-level bounds on size, shape, and prevalence to create synthetic rocks with molecular structures that closely resemble those found in natural formations.

Structural Attributes
Layered dipping facies altered by a range of structural features, including
Faults
Joints
Intrusions
Folds
Cleavage
and much more
