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Deep learning-based inversion with discrete cosine transform discretization for two-dimensional basement relief imaging of sedimentary basins from observed gravity anomalies

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dc.creator Ai, Hanbing
dc.creator Ekinci, Yunus Levent
dc.creator Roy, Arka
dc.creator BALKAYA, Çağlayan
dc.date 2025-01-01T00:00:00Z
dc.date.accessioned 2025-02-25T10:33:59Z
dc.date.available 2025-02-25T10:33:59Z
dc.identifier 8dfea2fc-b4e4-4b7a-8c55-8f9bbc1d52ff
dc.identifier 10.1111/1365-2478.13647
dc.identifier https://avesis.sdu.edu.tr/publication/details/8dfea2fc-b4e4-4b7a-8c55-8f9bbc1d52ff/oai
dc.identifier.uri http://acikerisim.sdu.edu.tr/xmlui/handle/123456789/100526
dc.description Sedimentary basins, integral to Earth's geological history and energy resource exploration, undergo complex changes driven by sedimentation, subsidence and geological processes. Gravity anomaly inversion is a crucial technique offering insights into subsurface structures and density variations. Our study addresses the challenge of complex subsurface structure assessment by leveraging deep neural networks to invert observed gravity anomalies. Optimization approaches traditionally incorporate known density distributions obtained from borehole data or geological logging for inverting basement depth in sedimentary basins using observed gravity anomalies. Our study explores the application of deep neural networks in accurate architectural assessment of sedimentary basins and demonstrates their significance in mineral and hydrocarbon exploration. Recent years have witnessed a surge in the use of machine learning in geophysics, with deep learning models playing a pivotal role. Integrating deep neural networks, such as the feedforward neural networks, has revolutionized subsurface density distribution and basement depth estimation. This study introduces a deep neural network specifically tailored for inverting observed gravity anomalies to estimate two-dimensional basement relief topographies in sedimentary basins. To enhance computational efficiency, a one-dimensional discrete cosine transform based discretization approach is employed. Synthetic data, generated using non-Gaussian fractals, compensates for the scarcity of true datasets for training the deep neural network model. The algorithm's robustness is validated through noise introduction with comparisons against an efficient and traditional global optimization-based approach. Gravity anomalies of real sedimentary basins further validate the algorithm's efficacy, establishing it as a promising methodology for accurate and efficient subsurface imaging in geological exploration.
dc.language eng
dc.rights info:eu-repo/semantics/closedAccess
dc.title Deep learning-based inversion with discrete cosine transform discretization for two-dimensional basement relief imaging of sedimentary basins from observed gravity anomalies
dc.type info:eu-repo/semantics/article


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