Buda Limestone

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Buda Limestone
Stratigraphic range: Late Cretaceous
Cenomanian
Type
Woodbine Formation, Boquillas Formation
OverliesDel Rio Formation and Grayson Formation
Thickness100 feet (30 m)
Lithology
PrimaryLimestone
Location
Coordinates30°05′06″N 97°51′03″W / 30.0849°N 97.8507°W / 30.0849; -97.8507
RegionNorth America
CountryUnited States
Type section
Named forBuda, Texas
Named byT.W. Vaughan
Year defined1900
Buda Limestone is located in the United States
Buda Limestone
Buda Limestone (the United States)
Buda Limestone is located in Texas
Buda Limestone
Buda Limestone stratigraphic column in Texas

The Buda Limestone is a geological

formation in the High Plains and Trans-Pecos regions of West Texas[1] and in southern New Mexico,[2] whose strata date back to the Late Cretaceous. Pterosaur remains are among the fossils that have been recovered from the formation.[3]

Description

Terlingua stratigraphic column – Buda Limestone

The Buda Limestone is a dense white to yellow sparry limestone with numerous calcite veins that weathers to yellowish or pinkish due to its iron content. In far western Texas, the formation overlies the Del Rio Formation and is in turn overlain by the Eagle Ford Group. The total thickness is about 100 feet (30 m).[1][4] In trans-Pecos Texas, the formation rests on the Grayson Formation and is overlain by the Boquillas Formation.[5]

In the

argillaceous or marly nodular grayish-white limestone. The upper member is up to 60 feet (18 m) of limestone similar to the lower member.[6]

Fossils

Alectryonia carinata[1] has also been found in the formation. Abundant bivalve fossils are found in the formation east of Big Bend National Park.[6]

Exposures in Hays County, Texas have yielded fossil remains of Pterodactyloidea, Ornithocheiroidea and Ornithocheiridae.[3]

Type locality for Graptocarcinus texanus Roemer, 1887[7](Decapoda: Brachyura).

Economic resources

The Buda Limestone is an important

horizontal and underbalanced drilling.[8] While the vertical wells relied on the porosity of the formation (up to 6%), the horizontal wells exploit a system of natural vertical fractures in the formation.[9]

History of investigation

The formation was originally named the Shoal Creek Limestone, but this name was preempted, and the formation was renamed the Buda Limestone by T.W. Vaughan in 1900.[1] By 1935, the formation had been included in the Washita Group.[10]

See also

References

  1. ^ a b c d e Vaughan, T.W. (1900). "Reconnaissance in the Rio Grande coal fields of Texas, including a report on igneous rocks from the San Carlos coal field by C.E. Lord" (PDF). U.S. Geological Survey Bulletin. 164. Retrieved 11 September 2020.
  2. ^ a b Lovejoy, E.M.P. (1976). "Geology of Cerro de Cristo Rey uplift, Chihuahua and New Mexico" (PDF). New Mexico Bureau of Mines and Mineral Resources Memoir. 31. Retrieved 3 August 2020.
  3. ^ a b Barrett, P.M., Butler, R.J., Edwards, N.P., & Milner, A.R. Pterosaur distribution in time and space: an atlas. p61-107. in Flugsaurier: Pterosaur papers in honour of Peter Wellnhofer. 2008. Hone, D.W.E., and Buffetaut, E. (eds). Zitteliana B, 28. 264pp.[1]
  4. doi:10.1190/tle35090752.1
    . Retrieved 12 September 2016.
  5. S2CID 140622822
    .
  6. ^ a b Barnes, V.E. (1977). Geologic atlas of Texas. University of Texas-Austin, Bureau of Economic Geology.
  7. ^ Roemer, F.A. (1887). "Graptocarcinus texanus, ein Brachyure aus der Kreide von Texas". Neues Jahrbuch für Mineralogie, Geologie, und Paläontologie. 1887: 173–176.
  8. doi:10.2118/179715-MS
    .
  9. ^ Ledoux, R; Gottardi, R. (2018). "Characterizing the Natural Fracture System of the Buda Formation, South Texas". Gulf Coast Association of Geological Societies Transactions. 68: 605–610.
  10. ^ Wilmarth, M.G. (1938). "Lexicon of geologic names of the United States (including Alaska)". U.S. Geological Survey Bulletin. 896.
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