Pg. D42-D43. Dye Shale Member of Bloyd Shale. Predominantly dark-gray to black shaly siltstone and claystone. Thin lenticular limestone beds and calcareous zones present locally. Basal unit is referred to as "caprock of the Baldwin coal." Thickness 60 to 110 feet. Overlies Woolsey Member; underlies Kessler Limestone Member. Age is Early Pennsylvanian (Morrow).
Type locality: from E/2 sec. 3 to center of north side sec. 4, T. 14 N., R. 30 W., Washington Co., northwestern AR. Named from Dye Creek.
Source: US geologic names lexicon (USGS Bull. 1350, p. 229).
Pg. A10-A11, A54, A56-A57 (fig. 5). Dye Shale Member of Bloyd Formation or Bloyd Shale. Present in northwest Ozark region, Arkansas. Age changed from Early Pennsylvanian (Morrowan) to: Middle Pennsylvanian (Morrowan; early Westphalian A of Europe); foram zone 20 and ammonoid zone AXINOLOBUS MODULUS. [See also Mackenzie Gordon, Jr., and G.C. Stone, 1976, Arkansas Geol. Commission Symposium on the geology of the Ouachita Mountains, v. 1.]
Source: Publication.
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