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- W2045184589 abstract "Summary Exposed Ordovician strata in the western Tarim Basin in Northeastern China show a karst system that consists of karst towers and paleocave breccias. These outcrops are used to build 3D geocellular model and 3D synthetic seismogram. The low impedance paleocave breccias create distinctive high amplitude seismic anomalies below the unconformity reflection. A larger model is built with the top Ordovician surface mapped in the subsurface and with randomly distributed ellipses to simulate the paleocaves. The resulting seismograms show realistic reflection character and geometries. Impedance model with 150 m to 250 m wide by at least 20m thick paleocaves with a 175 % impedance contrast between the paleocave and host rock results in 3D synthetic seismogram that mimic the amplitude anomalies observed in the subsurface data." @default.
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- W2045184589 date "2010-01-01" @default.
- W2045184589 modified "2023-10-10" @default.
- W2045184589 title "An Ultra‐Deep Paleokarst System in the Ordovician, North‐Central Tarim Basin, China: Outcrop analog and synthetic seismic models" @default.
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- W2045184589 doi "https://doi.org/10.1190/1.3513132" @default.
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