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Version:
2024.1.1
Salvus documentation version
2024.1.1
2024.1.0
0.12.16
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GETTING STARTED
Installation
Where to Run Things?
Python Packages
Mondaic Downloader
SalvusFlow Configuration
Config Builder
Example Site Configurations
Advanced Topics
Apple M-Series chips
Windows
Windows Subsystem for Linux
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SSH Configuration
MPI
Proxy Configuration
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Release Notes for Salvus 2024.X
Older Versions
Release Notes for Salvus 0.11.X
Knowledge Base
Wave Equation
Boundary Conditions
Natural Boundary Conditions
Homogeneous Dirichlet
Absorbing Boundaries
Mesh Generation
Spectral-Element Modelling
Dispersion Error
Wavefield Separation
Parameterizations
Units
Inverse Problems
Velocity Misfits
Gradient Misfits
Examples & Tutorials
Tutorials
Getting Started
First Steps
Part 1 - My first simulation
Part 2 - My first inversion
Next Steps
Part 1 - First simulation
Part 2 - Verification
Part 3 - Visualization
Part 4 - Heterogeneous models
Models and topography
Model order
Parameterizations
Simple topography
Layered models
Heterogeneous models and slice extraction
Marmousi
3D surface topography
Meshing
Meshing of layered models
Part 1 - Basics
Part 2 - Basics: Partitioning and Policies
Part 3 - Meshing complex geophysical domains
Importing external meshes
Mesh-to-mesh interpolation
Cylindrical meshes
Data-adaptive mesh masking
Sources and receivers
Introduction
Locating sources and receivers
Custom source time functions
Equivalence of filtering STFs and filtering synthetics
Waveform physics
Attenuation
Acoustic VTI
2D teleseismic simulation
Ocean loading
Data analysis
Receiver Gathers
Wavefield Output
Inversion
Full-waveform inversion
Part 1 - Setup
Part 2 - Synthetics
Part 3 - Sensitivities
Part 4 - Iterations
Part 5 - Extensions
Gradient preconditioning
Smoothing
Homogeneous media
Gradients for Seismology
Advanced Interface
Lamb's problem
Model interpolation
SalvusFlow API
Manual gradient computation
Marmousi
Applications
Seismology
Continental-scale simulations
Sensitivity kernels
Global-scale simulation
Geotech
Ground motion modeling of buildings
Real data continental-scale FWI
Part 0 - Prologue
Part 1 - Project setup & data acquisition
Part 2 - Forward simulations
Part 3 - Data selection and misfit definition
Part 4 - Iterative inversion
Near Surface
Part 0 - Prologue
Part 1 - Project setup & importing external data
Part 2 - Starting Model
Part 3 - 3D-to-2D Conversion
Integration Tests
Analytic Tests
Semi-analytic test - Acoustic
Semi-analytic test - Elastic
Semi-analytic test - Coupled
On-the-fly Fourier transform
Analytic test - Diffusion equation
Analytic test - Poisson's equation
Gradient Tests
Gradient test simple physics
Gradient test TTI medium
Reference Documentation
SalvusCompute API
SalvusMesh Interfaces
Cartesian2D
Cartesian3D
Cartesian2DHomogeneous
Cartesian3DHomogeneous
Circular2D
Globe3D
SmoothieSEM
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Python API
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hdf5_data_backend
segy_data_backend
xarray_data_backend
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event_data
event_data_collection_proxy
event_misfit
event_misfit_collection
event_window_and_weight_set
receiver_channel
types
wavefield_compression
executors
base_executor
executor_utils
functions
implementations
grid_engine
local
lsf
pbs
slurm
ssh
local_hpc
job
remote_io_executor
salvus_job
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types
functions
simple_config
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receiver
cartesian
collections
seismology
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source
transformations
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dim2
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dim2
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mask_generators
optimize_dt
point_sorting
spherical
tensorized_elements
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basic
deformations
extrude
io
metrics
parallel_utils
refinements
side_sets
utils
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mesh_block_collection
unstructured_mesh
unstructured_mesh
layered_meshing
detail
detail
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coordinate_systems
special_cases
smoothiesem
mesh_from_domain
realize
interface
curve
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layered_model
bm
detail
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flood
split_layered_model
simple_mesh
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tools
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modules
near_surface
processing
geophone_response
point_to_line_source_conversion
source_inversion
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waveform_db
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namespace
opt
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l2_energy_per_measurement
normalized_misfit
iteration
mappings
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methods
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trustregion
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PUBLICATIONS
python_api
/
salvus
/
material
/
acoustic
/
transversely_isotropic
/
dim3
salvus.material.acoustic.transversely_isotropic.dim3
3-D anisotropic acoustic materials.
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GETTING STARTED
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