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- W1521049049 abstract "The Michigan basin has been sampled extensively by boreholes. Phanerozoic units thicken toward the center of the basin in sub-circular isopach patterns. General concordance of isopach and facies patterns with deeper-water facies occupying the basin interior indicate subsidence of the basin concomitant with deposition. Three regional unconformities, corresponding to the boundaries of craton-wide stratigraphic sequences (Sauk, Tippecanoe, Kaskaskia) interrupt the Paleozoic stratigraphy of the basin and represent basin-wide cessations of subsidence followed by renewed downwarp. The cause of basin subsidence is not yet well understood; surficial loading is inadequate to explain the magnitude of subsidence and at least two heating events (Cambrian and pre-Middle Ordovician) would be required if thermal contraction of the lithosphere is invoked. Deep drilling has found no direct evidence of a post-Cambrian thermal event. Petroleum exploration and studies of borehole samples will probably continue at a steady pace in the Michigan basin. Integration of resulting new data with published stratigraphic and sedimentologic information will be a prerequisite to the presentation of “hard” data in a form usable by geophysicists." @default.
- W1521049049 created "2016-06-24" @default.
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- W1521049049 date "2013-03-15" @default.
- W1521049049 modified "2023-10-17" @default.
- W1521049049 title "The Michigan Basin" @default.
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- W1521049049 doi "https://doi.org/10.1029/gd001p0093" @default.
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