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SEISMIC LINE A
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Fig. 9.44. A typical seismic line through the Fort Union Formation, Powder River Basin, Wyoming. The Lower Fort Union (LFU) shows a gradation from low-continuity, lowamplitude, low-frequency fluvial strata at left, through high-frequency, east�dipping clinoform shoreline deposits, to lacustrine deposits at lower right of unit. (Ray 1982,
reprinted by permission)
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SEISMIC LINE A
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Fig. 9.44. A typical seismic line through the Fort Union Formation, Powder River Basin, Wyoming. The Lower Fort Union (LFU) shows a gradation from low-continuity, lowamplitude, low-frequency fluvial strata at left, through high-frequency, east�dipping clinoform shoreline deposits, to lacustrine deposits at lower right of unit. (Ray 1982,
reprinted by permission)
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