The experiment aims to investigate the electronic configurations, structural transitions, and magnetism in iron Fe4O5 utilizing the Synchrotron Mössbauer Source spectroscopy and Single-Crystal X-ray d
Seismic impedance inversion is a geophysical technique that transforms seismic data into quantitative subsurface properties, primarily acoustic impedance. This process enables the identification of ro
The directory contains velocity models from OpenFWI dataset collection. These velocity models are the inputs of the FNO-based sovlers in the paper Solving Seismic Wave Equation on Variable
Seismic impedance inversion is a geophysical technique that transforms seismic data into quantitative subsurface properties, primarily acoustic impedance. This process enables the identification of ro
