Abstract

Deep learning has become an area of interest in most scientific areas, including physical sciences. Modern networks apply real-valued transformations on the data. Particularly, convolutions in convolutional neural networks discard phase information entirely. Many deterministic signals, such as seismic data or electrical signals, contain significant information in the phase of the signal. We explore complex-valued deep convolutional networks to leverage non-linear feature maps. Seismic data commonly has a lowcut filter applied, to attenuate noise from ocean waves and similar long wavelength contributions. In non-stationary data, the phase content can stabilize training and improve the generalizability of neural networks. While it has been shown that phase content can be restored in deep neural networks, we show how including phase information in feature maps improves both training and inference from deterministic physical data. Furthermore, we show that smaller complex networks outperform larger real-valued networks.

Highlights

  • While it has been shown that phase content can be restored in deep neural networks, we show how including phase information in feature maps improves both training and inference from deterministic physical data

  • We show that including explicit phase information provides superior results to real-valued convolutional neural networks for seismic data

  • The inclusion of phase-information leads to a better representation of seismic data in convolutional neural networks

Read more

Summary

Methods

The data is the F3 seismic data, interpreted by Alaudah et al [2019]. They provide a seismic benchmark for machine learning with accessible NumPy format. The interpretation (labels) of the seismic data is relatively coarse compared to conventional seismic interpretation, but the accessibility and pre-defined test case are compelling. The F3 data set was acquired in the Dutch North Sea in 1987 over an area of 375.31 km. The sampling-rates are 4 ms in time and inline/crossline bins of 25 m. The extent being 650 inline traces and 950 crossline traces with a total length of 1.848 s. The data contains faulted reflector packets, of which the lowest one overlays a salt diapir. The data contains some noise that masks lower-amplitude events

Results
Discussion
Conclusion
Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.