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Gilman Conglomerate

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A geologic formation in New Mexico
Gilman Conglomerate
Stratigraphic range: Oligocene PreꞒ O S D C P T J K Pg N
Gilman Conglomerate at Gilman, New Mexico
TypeFormation
UnderliesAbiquiu Formation
OverliesAbo Formation
Thickness59 m (194 ft)
Lithology
PrimaryConglomerate
Location
Coordinates35°43′03″N 106°46′01″W / 35.7175607°N 106.7669774°W / 35.7175607; -106.7669774
RegionNew Mexico
CountryUnited States
Type section
Named forGilman (settlement)
Named byKelley et al.
Year defined2009
Gilman Conglomerate is located in the United StatesGilman ConglomerateGilman Conglomerate (the United States)Show map of the United StatesGilman Conglomerate is located in New MexicoGilman ConglomerateGilman Conglomerate (New Mexico)Show map of New Mexico

The Gilman Conglomerate is a geologic formation in northern New Mexico dating to the Oligocene epoch.

Description

The formation is composed of poorly sorted, weakly bedded, greenish-gray volcaniclastic conglomerate. Its lowermost and uppermost sections are a pinkish color from their content of Proterozoic pebbles, but the bulk of the formation is dominated by a mixture of crystal-rich porphyritic dacite and crystal-poor porphyritic andesite. Radiometric dating yields ages of 28.55 to 29.38 Ma for the clasts. Paleocurrents are to the north, suggesting a source in an Oligocene volcanic field now buried under the southern Jemez Mountains or in the northern Albuquerque Basin.

The formation crops out in a limited area of the southwestern Jemez Mountains. Maximum thickness is 59 meters (194 feet).

The formation rests unconformably on the Abo Formation and has a gradational contact with the overlying Abiquiu Formation. It occupies the same stratigraphic position as the Ritito Conglomerate, and was originally included in that formation, but its composition and paleocurrent directions point to a quite different source provenance.

History of investigation

The unit was originally included in the Ritito Conglomerate by H.R. DuChene in 1973. It was broken out as a separate formation by Shari Kelley and her coinvestigators in 2009.

Footnotes

  1. ^ Osburn et al. 2002.
  2. ^ Maldonado & Kelley 2009.
  3. DuChene 1973.
  4. Kelley et al. 2009.

References

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