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- W1511590623 abstract "Within the study area, the Boyles Sandstone Member is overlain by a thick, gray, siliciclastic sequence ranging progressively from fine-grained shales and coal of interdistributary bay-fill sequences to tightly cemented channel sandstones that contain carbonaceous debris above basal pebble conglomerates. Overlying the bay-fill sequences are poorly cemented fluviodeltaic sandstones that are pink to red and well cemented along the basal contact with the gray shales or gray clay. The unconsolidated to friable sands are exposed below the Cretaceous unconformity in the study area. This succession of lithologies reflects the southward progradation of the Pottsville deltaic complex during the Early Pennsylvanian. During this time, the deltaic system prograded over the underlying East Warrior platform." @default.
- W1511590623 created "2016-06-24" @default.
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- W1511590623 date "1988-08-01" @default.
- W1511590623 modified "2023-09-27" @default.
- W1511590623 title "Stratigraphy within Lower Pottsville Formation of Alabama" @default.
- W1511590623 hasPublicationYear "1988" @default.
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