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Mineral Fork Formation

From Wikipedia, the free encyclopedia

Mineral Fork Formation
Stratigraphic range: Proterozoic
Diamictite Mineral Fork.JPG
Boulder of diamictite of the Mineral Fork Formation, along the Elephant Head Trail, Antelope Island, Utah.
Typesedimentary
UnderliesMutual Formation (Big Cottonwood Canyon), Tintic Formation (Santaquin-Provo), or Kelly Canyon Formation (Antelope Island)[1]
OverliesFarmington Canyon Complex (Antelope Island), Big Cottonwood Formation (other locations)[1]
Thickness1000 to 3000 feet
Lithology
PrimaryTillite, Shale, Quartzite, Conglomerate
Location
RegionSouthern Rocky Mountains
ExtentWasatch Mountains, Antelope Island
Type section
Named forMineral Fork, Salt Lake County, Utah
Named byGranger et al., 1952[2]

The Mineral Fork Formation is a mapped Proterozoic bedrock unit in Utah.

Description

Granger et al. (1952) describe the Mineral Fork Formation as black tillite consisting of boulders, cobbles and pebbles of quartzite, limestone, or granitic rocks in a black sandy matrix, with dark-gray to black varved slate or shale, dark-gray quartzite, and occasional channel fillings of boulder conglomerate.[2]

Exposures

According to Yonkee et al. (2000), the Mineral Fork is exposed at the following locations in Utah:[1]

And also:

Fossils

Abundant microfossils of planktonic alga of Bavlinella faveolata.[3]

Age

The presence of Bavlinella faveolata in the formation indicates a likely age of 750–650 Ma, because this fossil occurs elsewhere where it is well-dated radiometrically. The Mineral Fork Formation is no older than 1,250 Ma and no younger than 540 Ma. Thus it is likely Neoproterozoic but possibly Mesoproterozoic.[3]

References

  1. ^ a b c Yonkee, W.A, Willis, G.C., and Doelling, H.H., 2000, Proterozoic and Cambrian Sedimentary and Low-grade Metasedimentary Rocks on Antelope Island, in The Geology of Antelope Island, Davis County, Utah, eds. J.K. King and G.C. Willis, Utah Geological Survey, p. 37–47.
  2. ^ a b Granger, A.E., Calkins, F.C., Crittenden, M.D., Jr., and Sharp, B.J., 1952, Geology of the Wasatch Mountains east of Salt Lake City, IN Marcel, R.E., ed., Geology of the central Wasatch Mountains, Utah: Utah Geological Society, Guidebook to the geology of Utah, no. 8, p. 1-37.
  3. ^ a b Knoll, A.H., Blick, N., and Awramik, S.M., 1981, Stratigraphic and ecologic implications of late Precambrian microfossils from Utah: American Journal of Science, v. 281, no. 3, p. 247-263.
This page was last edited on 19 March 2021, at 19:38
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