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Map showing publication footprint
  • Usage in publication:
    • Neylandville marl*
  • Modifications:
    • Biostratigraphic dating
  • AAPG geologic province:
    • East Texas basin
Publication:

Cooke, C.W., 1953, American Upper Cretaceous Echinoidea, IN Shorter contributions to general geology, 1953: U.S. Geological Survey Professional Paper, 254-A, p. A1-A44.


Summary:

Is basal formation of Navarro group. Overlies Taylor marl. Underlies Nacatoch sand of Navarro group. Is shown (on fig. 1) to correlate with Saratoga chalk in AR and with Mount Laurel sand in NJ. Biostratigraphic dating on basis of the Maestrichtian echinoid HEMIASTER WETHERBYI De Loriol recorded from the Neylandville at USGS locality 15523, 2.5 mi air line south of Ben Hur, Limestone Co, TX in East Texas basin. Age is early Maestrichtian (Late Cretaceous). Division of the Maestrichtian into three parts (early, middle, and late) is arbitrary. It signifies merely relative position.

Source: GNU records (USGS DDS-6; Denver GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Neylandville Formation
  • Modifications:
    • Mapped 1:250k
  • Dominant lithology:
    • Clay
  • AAPG geologic province:
    • East Texas basin
Publication:

Barnes, V.E. (project director), 1966, Geologic atlas of Texas, Texarkana sheet: University of Texas-Austin, Bureau of Economic Geology Geologic Atlas of Texas, 1 sheet, scale 1:250,000, Elias H. Sellards memorial edition


Summary:

Neylandville Formation. Clay, calcareous, silty, sandy, medium-gray; weathers light-gray, forms somewhat irregular topography; scattered marine megafossils. Thickness 752 feet, feathers out eastward. Lies above Marlbrook Marl and below Navarro Group, undivided. Age is Late Cretaceous.
[Mapped in central western part of map sheet, btw. North Sulphur and South Sulphur Rivers, in Delta and Hunt Cos., northeastern TX.]

Source: Publication.


Map showing publication footprint
  • Usage in publication:
    • Neylandville Formation
  • Modifications:
    • Areal extent
  • AAPG geologic province:
    • East Texas basin
    • Gulf Coast basin
Publication:

Barnes, V.E. (project director), 1970, Geologic atlas of Texas, Waco sheet: University of Texas-Austin, Bureau of Economic Geology Geologic Atlas of Texas, 1 sheet, [9 p.], scale 1:250,000, Lloyd William Stephenson memorial edition


Summary:

Neylandville Formation. Lies above Marlbrook Marl ("upper Taylor marl") and below Kemp Clay. Age is Late Cretaceous.
Not separately mapped. (Neylandville and Marlbrook [undifferentiated] mapped in Falls, Hill, Limestone, McLennan, Milam, and Navarro Cos., eastern TX.)

Source: Publication.


Map showing publication footprint
  • Usage in publication:
    • Neylandville Formation
  • Modifications:
    • Mapped 1:250k
  • Dominant lithology:
    • Clay
    • Sand
  • AAPG geologic province:
    • East Texas basin
    • Ouachita folded belt
Publication:

Barnes, V.E. (project director), 1987, Geologic atlas of Texas, Dallas sheet [revision of 1972 ed.]: University of Texas-Austin, Bureau of Economic Geology Geologic Atlas of Texas, 1 sheet, [10 p., revised 1988], scale 1:250,000, Gayle Scott memorial edition


Summary:

Neylandville Formation. Clay, calcareous, silty, sandy, sand content increases upward, medium gray; weathers light gray, forms irregular topography. Thickness 125+/- feet. Lies above Marlbrook Marl ("upper Taylor marl") and below Nacatoch Sand. Age is Late Cretaceous.
[Mapped in Collin, Hunt, and Rockwall Cos., eastern TX.]

Source: Publication.


Map showing publication footprint
  • Usage in publication:
    • Neylandville Formation
  • Modifications:
    • Mapped 1:250k
  • Dominant lithology:
    • Clay
  • AAPG geologic province:
    • East Texas basin
    • Ouachita folded belt
Publication:

Barnes, V.E. (project director), 1991, Geologic atlas of Texas, Sherman sheet [revision of 1967 ed.]: University of Texas-Austin, Bureau of Economic Geology Geologic Atlas of Texas, 1 sheet, [17 p.], scale 1:250,000, Walter Scott Adkins memorial edition


Summary:

Pamphlet [p. 2]. Neylandville Marl. Clay, medium-gray, weathers to light-gray, calcareous, silty, sandy; forms irregular topography; marine megafossils scarce. Thickness approximately 75 feet. Lies below Navarro Group and above Marlbrook Marl. Age is Late Cretaceous.
[Mapped in southeastern corner of map sheet, in Hunt and Collins Cos., northeastern TX.]

Source: Publication.


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