Publication | Closed Access
Deep Relative Geologic Time: A Deep Learning Method for Simultaneously Interpreting 3‐D Seismic Horizons and Faults
75
Citations
59
References
2021
Year
Geometric LearningConvolutional Neural NetworkEngineeringMachine LearningRgt VolumeGeological ModelingEarth ScienceGeophysicsImage AnalysisData ScienceEarthquake SourceImage-based ModelingComputational ImagingGeophysical InterpretationDeep Learning MethodGeographySeismic ImagingSimultaneously Interpreting 3‐DGeologyDeep LearningTectonicsAbstract Extracting HorizonsFault GeometrySeismologySeismic HorizonsRgt VolumesFoundation Models
Abstract Extracting horizons and detecting faults in a seismic image are basic steps for structural interpretation and important for many seismic processing schemes. A common ground of the two tasks is to analyze seismic structures and they are related to each other. However, previously proposed methods deal with the tasks independently, and challenge remains in each of them. We propose a volume‐to‐volume neural network to estimate a relative geologic time (RGT) volume from a seismic volume, and this RGT volume is further used to simultaneously interpret horizons and faults. The network uses U‐shaped framework with attention mechanism to systematically aggregate multi‐scale information and automatically highlight informative features, and achieves high prediction accuracy with affordable computational costs. To train the network, we build thousands of 3‐D noisy synthetic seismic volumes and corresponding RGT volumes with realistic and various structures. We introduce a loss function based on structure similarity to capture spatial dependencies among seismic samples for better optimizing the network, and use multiple reasonable assessments to evaluate the predicted results. Trained by using synthetic data, our network outperforms the conventional approaches in recognizing structural features in field data examples. Once obtaining an RGT volume, we can not only obtain seismic horizons by simply extracting RGT constant surfaces but also detect faults that are indicated by lateral RGT discontinuities. To be able to deal with large seismic volumes, we further propose a workflow to first estimate sub‐volumes of RGT and merge them to obtain a full RGT volume without boundary artifacts.
| Year | Citations | |
|---|---|---|
Page 1
Page 1