251. Automatic fault detection in seismic data using Gaussian process regression.
- Author
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Noori, Maryam, Hassani, Hossein, Javaherian, Abdolrahim, Amindavar, Hamidreza, and Torabi, Siyavash
- Subjects
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KRIGING , *RANDOM noise theory , *RECEIVER operating characteristic curves , *GAUSSIAN processes , *SIGNAL-to-noise ratio , *SALT domes , *GEOLOGIC faults , *SEISMOLOGY - Abstract
Compartmentalization of hydrocarbon reservoirs, change in fluid contacts, effects of high permeable fractures around faults, and hydrocarbon traps created by seal faults make fault detection and extraction as a necessity in the analysis of seismic data. Faulting disrupts the smoothness trend of geological layers (reflections in seismic sections) and displaces layers along its plane. Thus, a fault could be considered as an abnormal phenomenon that globally deviates normal behavior of layers around its plane. In the present study, faults are considered as sparse global anomalies in a seismic section that can be extracted using Gaussian process regression. The Gaussian process regression is a nonparametric probabilistic model based on Bayesian statistics that can be used to model spatial properties as a regression problem. The Gaussian process usually is used to extract and describe normal interactions from the data set using smooth functions. The main idea of this study is to detect the global anomaly using Gaussian process regression. For this purpose, we considered geological layers as smooth normal events in seismic sections. Therefore, the location of the fault plane is where the Gaussian process gets an error during describing the layers. Abnormalities such as faults cause the Gaussian process to suffer an error near the anomaly. We used these errors and analyzed them to detect probable locations of fault edge. Finally, we used a consistent connection algorithm to separate most probable fault points and to connect them to an edge using morphological reconstruction algorithm. The proposed algorithm was evaluated based on the receiver operating characteristics analysis. Several synthetic seismic sections with different levels of signal to noise ratios were used to evaluate the algorithm in the presence of random noise. The results showed that all points predicted by a diagnostic test fell into the area above the diagonal of the receiver operating characteristics space, which represents a good diagnostic classification. • Faulting disrupts the smoothness trend of geological layers. • Global anomaly in a data set is an abnormal phenomenon that globally deviates normal behavior of data set. • Fault and salt dome boundary could be considered as an abnormal phenomenon in seismic data. • The Gaussian process usually is used to extract and describe normal interactions from the data. • Fault locations is where the Gaussian process gets an error during describing the layers as normal events. [ABSTRACT FROM AUTHOR]
- Published
- 2019
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