Depth migration and interpretation of the COCORP Wind River, Wyoming, seismic reflection data

摘要: To better understand Laramide deformation, deep seismic reflection data have been depth migrated (focused or imaged) in order to more clearly reveal structural features associated with the Wind River thrust, Wyoming. Major displayed are fault zone and Pacific Creek anticline. The is seen a of at least 25 km interpretively 32 km. It complex that includes numerous splays flattening depth. Range was tilted along these arcuate as it compressionally thrust up. anticline asymmetric cored, top basement offset 600 m. viewed an embryonic thrust.