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Bisbee Group

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Bisbee Group
Stratigraphic range: early Cretaceous
TypeGroup
Sub-unitsGlance Conglomerate, Morita Formation, Mural Limestone, Cintura Formation
UnderliesBronco Volcanics
OverliesNaco Formation
ThicknessOver 21,000 feet (6,400 m)
Lithology
PrimarySandstone, claystone, limestone
OtherConglomerate
Location
Coordinates31°25′N 109°57′W / 31.42°N 109.95°W / 31.42; -109.95
RegionArizona
New Mexico
Chihuahua
CountryUnited States
Mexico
Type section
Named byE.T. Dumble
Year defined1902
Bisbee Group is located in the United States
Bisbee Group
Bisbee Group (the United States)
Bisbee Group is located in Arizona
Bisbee Group
Bisbee Group (Arizona)

The Bisbee Group is a geologic group in Arizona,[1] Mexico, and New Mexico.[2] It preserves fossils dating back to the early Cretaceous period.[3]

Description

The group consists of sandstone, claystone, limestone, and conglomerate,[1] with a total thickness of 4,750 feet (1,450 m).[3] In the Tombstone, Arizona, area, it overlies the Naco Formation.[4] In the Bisbee area, the group is divided into four formations, which in ascending stratigraphic order are the Glance Conglomerate, the Morita Formation, the Mural Limestone, and the Cintura Formation.[3] The group is overlain by the Bronco Volcanics,[5] the Nipper Formation, or the Faraway Ranch Formation.[6][2]

In southwestern New Mexico, the group thickens to 21,000 feet (6,400 m) and is divided into the Glance Conglomerate, the Hell-to-Finish Formation, the U-Bar Formation, and the Mojado Formation.[7][8][9][2]

Fossils

The group contains fossils such as the mollusc Exogyra and the clam Trigonia characteristic of the Cretaceous.[1]

History of investigation

The Bisbee beds were first named by E.T. Dumble in 1902 for exposures around Bisbee, Arizona.[1] In 1904, Frederick Leslie Ransome divided the Bisbee Group into formations in the Bisbee area.[3] By 1938, the group had been mapped into the Tombstone, Arizona area[4] and into southwestern New Mexico.[7] Samuel G. Lasky defined several new formations within the group, but some of these were synonyms for each other due to fault doubling.[8]

See also

References

  • Butler, B.S.; Wilson, E.D.; Rasor, C.A. (1938). "Geology and ore deposits of the Tombstone district, Arizona". Arizona Bureau of Mines Bulletin. 143. Retrieved 10 September 2020.
  • Drewes, Harald (1991). "Geologic map of the Big Hatchet Mountains, Hidalgo County, New Mexico". U.S. Geological Survey Report. doi:10.3133/i2144.
  • Dumble, E.T. (1902). "Notes on the geology of southeastern Arizona". American Institute of Mining and Metallurgical Engineers Transactions. 31: 103–105.
  • Gilluly, J. (1 December 1945). "Emplacement of the Uncle Sam porphyry, Tombstone, Arizona". American Journal of Science. 243 (12): 643–666. Bibcode:1945AmJS..243..643G. doi:10.2475/ajs.243.12.643.
  • Lasky, Samuel G. (1938). "Newly Discovered Section of Trinity Age in Southwestern New Mexico". AAPG Bulletin. 22. doi:10.1306/3D932F80-16B1-11D7-8645000102C1865D.
  • Lawton, Timothy F. (2004). "Upper Jurassic and lower Cretaceous strata of southwestern New Mexico and Northern Chihuaua, 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.
  • Ransome, F.L. (1904). "The geology and ore deposits of the Bisbee quadrangle, Arizona". U.S. Geological Survey Professional Paper. Professional Paper. 21. doi:10.3133/pp21. hdl:2346/61697. Retrieved 10 September 2020.
  • Sabins, Floyd F. (1957). "Geology of the Cochise Head and Western Part of the Vanar Quadrangles, Arizona". Geological Society of America Bulletin. 68 (10): 1315. Bibcode:1957GSAB...68.1315S. doi:10.1130/0016-7606(1957)68[1315:GOTCHA]2.0.CO;2.
  • Zeller, R.A., Jr. (1970). "Geology of the Little Hatchet Mountains, Hidalgo and Grant Counties, New Mexico" (PDF). New Mexico Bureau of Mines and Mineral Resources Bulletin. 96. Retrieved 10 September 2020.{{cite journal}}: CS1 maint: multiple names: authors list (link)