1887

Abstract

Near vertical surfaces of sub-seismic faults, steep salt intrusion flanks, and fuzzy boundaries of fracture swarms relate to geologic objects that are difficult to image and characterize by conventional processing of seismic data. To solve the problem, a

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/content/papers/10.3997/2214-4609.201400572
2009-06-08
2021-10-16
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400572
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