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- W1841183059 abstract "Abstract Shelf carbonate mounds of Desmoines Pennsylvanian age are developed in cyclic repetition along the southwest flank of the Paradox basin. Optimum carbonate deposition occurred in an elongate northwest-southeast belt approximately 50 miles wide and at least 100 miles long. The belt contains about 35 Pennsylvanian oil and gas fields, all of which are productive from carbonate reservoirs. Porosity occurs in three types of carbonate buildup: algal-plate mounds, foraminiferal mounds or bioherms, and “leached oolite” banks. Most of the production is from limestones, but dolomites are also important. Stratigraphic mapping of the mound-bearing cycles can be done on the basis of basinwide sapropelic shale or dolomite marker beds which bound each cyclic layer. Shelf carbonates occur in each main cycle of the Paradox formation, grading basinward into evaporites and shoreward into sandy limestones and terrigenous clastics. The strongly cyclic conditions within the Paradox evaporitic depositional basin are thought to have been related to periodic eustatic sea level changes, probably associated with Late Paleozoic glacial cycles in the southern hemisphere." @default.
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- W1841183059 date "1963-01-01" @default.
- W1841183059 modified "2023-09-24" @default.
- W1841183059 title "Pennsylvanian Shelf Carbonates, Paradox Basin" @default.
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