Abstract:The Perdido fold belt, located in the northwest part of the Gulf of Mexico basin, is defined by a series of large-scale fold structures that extend southwest into Mexican waters and northeast beneath the Sigsbee salt nappe. Within the Alaminos Canyon OCS lease area, the fold belt consists of northeast-southwest trending, sub-parallel, concentric, box folds cut on one or both of their flanks by high-angle reverse faults. The folds are slightly asymmetric and verge both landward and basinward, a geometry typical… Show more
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