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- W2065403812 abstract "A deep (> 6 km) well, the Doubloon Saxon 1 well, drilled in early 1986 on the Great Bahamas Bank, shows evidence of massive seal failure through tectonic and post-tectonic diagenetic alteration. Seal failure occurred through a hydrodynamically induced chemical alteration of a carbonate (limestone, dolomite)-evaporite (anhydrite, halite) sequence into a carbonate (dolomite and dedolomite) sequence. Evidence for this alteration includes a thick (3.5 km) fractured dolomite sequence interbedded with dedolomites. Fracture origins include solution collapse (of original evaporites as shown by anhydrite cement on fracture surfaces) and cavernous porosity, and by tectonic fracturing (a major reverse fault penetrated with > 1 km repeat). Additional evidence includes a temperature regression and geochemical anomalies above and below the proposed altered sequence. It is concluded that massive seal failure is a contributing factor in limiting the petroleum potential of portions of the south-western Bahamas Platform." @default.
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- W2065403812 date "1993-02-01" @default.
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- W2065403812 title "Tectonic and diagenetically induced seal failure within the south-western Great Bahamas Bank" @default.
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- W2065403812 doi "https://doi.org/10.1016/0264-8172(93)90096-b" @default.
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