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The AAPG/Datapages Combined Publications Database
AAPG Bulletin
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Recent surveys have traced the belt of diapiric structures, first observed in the Sigsbee deep, through the Bay of Campeche to within about 60 mi of the saline basin of southeastern Mexico. This prompts a further examination of the structure of the Gulf of Mexico with particular attention to the possibilities that the diapirs are salt.
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