Queen Formation

The Queen Formation is a geologic formation in southeastern New Mexico and west Texas. It preserves fossils dating back to the late Guadalupian Epoch of the Permian period.[1][2]

Queen Formation
Stratigraphic range: Guadalupian
TypeFormation
Unit ofArtesia Group
UnderliesSeven Rivers Formation
OverliesSan Andres Formation
Thickness500 feet (150 m)
Lithology
PrimarySandstone
Otherdolomite, anhydrite
Location
Coordinates32.191°N 104.755°W / 32.191; -104.755
RegionNew Mexico
CountryUnited States
Type section
Named forQueen Post Office
Named byBlanchard and Davis
Year defined1929
Queen Formation (the United States)
Queen Formation (New Mexico)

Description

The formation consists of up[ to 500 feet (150 m)[3] of mostly sandstone, with some interbedded dolomite and anhydrite. It rests on the San Andres Formation, from which it is separated by an erosional surface showing karst features.[4] The Queen Formation is overlain by the Seven Rivers Formation. The Queen Formation is part of the Artesia Group, which is interpreted as a sequence of shelf rocks of the Capitan reef.[1][5]

History of investigation

The unit was first named as the Queen sandstone of the upper San Andres Formation by Blanchard and Davis in 1929[3] In 1937, Lang assigned the Seven Rivers Member to the (now abandoned) Chalk Bluff Formation.[6] The unit was promoted to formation rank and assigned to the Whitehorse Group by DeFord and Lloyd in 1940.[7] The foramtion was assigned to the Artesia Group by Tait et al. in 1962.[1]

See also

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Footnotes

  1. Tait et al. 1962
  2. Kues and Giles 2004, p. 100
  3. Blanchard and Davis 1929
  4. Kues and Giles 2004, p. 124-128
  5. Kues 2006
  6. Lang 1937
  7. Deford and Lloyd 1940

References

  • Blanchard, W. Grant; Davis, Morgan J. (1929). "Permian Stratigraphy and Structure of Parts of Southeastern New Mexico and Southwestern Texas". AAPG Bulletin. 13 (8): 957–995. doi:10.1306/3D93286E-16B1-11D7-8645000102C1865D.
  • DeFord, Ronald K.; Lloyd, E. Russel (1940). "West Texas-New Mexico Symposium: Part I Editorial Introduction". AAPG Bulletin. 24. doi:10.1306/3D933188-16B1-11D7-8645000102C1865D.
  • Kues, Barry S. (2006). "Geological studies of the Guadalupe Mountains area, New Mexico and West Texas, to 1928" (PDF). New Mexico Geological Society Field Conference Series. 57: 127–144. Retrieved 20 September 2020.
  • Kues, B.S.; Giles, K.A. (2004). "The late Paleozoic Ancestral Rocky Mountain system in New Mexico". In Mack, G.H.; Giles, K.A. (eds.). The geology of New Mexico. A geologic history: New Mexico Geological Society Special Volume 11. pp. 95–136. ISBN 9781585460106.
  • Lang, W.B. (1937). "The Permian formations of the Pecos Valley of New Mexico and Texas". American Association of Petroleum Geologists Bulletin. 21 (7): 833–898. doi:10.1306/3D932EDE-16B1-11D7-8645000102C1865D.
  • Tait, D.B.; Motts, W.S.; Spitler, M.E. (1962). "Artesia Group of New Mexico and West Texas". American Association of Petroleum Geologists Bulletin. 46 (4): 504–517. doi:10.1306/BC74383B-16BE-11D7-8645000102C1865D.
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