Improved imaging of carbonate caves in Tarim Basin using RFWI
Улучшенное изображение карбонатных пещер в Таримском бассейне с использованием RFWI
2026-02-10
SCID: 54.1/pxht8zbw
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Reflection Full Waveform Inversion (RFWI)Tarim Basincarbonate cave imaginghigh-velocity igneous and salt overburdenvelocity model updating
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Abstract (AI)
The imaging of carbonate caves in the Tarim Basin is challenging due to the lithological complexity of the overburden and the surrounding geology. The overburden consists of irregular igneous rocks, and salt layers, all showing high velocity contrasts, compared with the siliciclastic background rock. These irregularities significantly affect the image quality of the deeper structure, cave locations, and focusing characteristics. This study utilizes Reflection Full Waveform Inversion (RFWI) to update the velocity structure of the deep targets due to the lack of long offsets. Through RFWI, we achieved a higher resolution velocity model of the igneous layer, enhancing the imaging of deeper caves.
Key Findings
1
Improved igneous-layer velocity model enhanced imaging and focusing of deeper carbonate caves
2
Irregular igneous rocks and salt layers with high velocity contrasts in the overburden significantly degrade deep-structure and cave imaging
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RFWI produced a higher-resolution velocity model of the igneous overburden layer
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Reflection Full Waveform Inversion (RFWI) was used to update the velocity structure of deep targets in the Tarim Basin despite lack of long offsets
Research Object
Carbonate caves in the Tarim Basin
Research Subject
Improved seismic imaging (including cave locations, deeper structure and focusing) via velocity-updating using Reflection Full Waveform Inversion (RFWI) to resolve effects of irregular igneous and salt overburden
Publication Details
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2026-02-10
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