The Bar B Formation is a geologic formation found the Caballo Mountains of New Mexico. It preserves fossils showing it was deposited in the middle to late Pennsylvanian.[1][2]
Bar B Formation | |
---|---|
Stratigraphic range: | |
Type | Formation |
Underlies | Bursum Formation |
Overlies | Nakaye Formation |
Thickness | 339 ft (103 m) |
Lithology | |
Primary | Limestone, shale |
Location | |
Coordinates | 33°01′07″N 107°14′20″W / 33.0185°N 107.2390°W |
Region | New Mexico |
Country | United States |
Type section | |
Named for | Barbee Draw (drainage) |
Named by | V.C. Kelley and Caswell Silver |
Year defined | 1952 |
Description
editThe Bar B formation is mostly cyclic[2] beds of shale and limestone, with shale making up about 80% of the formation and limestone the other 20%. Chert is present in some of the limestone. The upper 50 feet (15 m) include reddish-brown siltstone, limestone conglomerate, and calcareous siltstone. The total thickness is about 339 ft (103 m).[3] The formation rests on the Nakaye Formation and is unconformably overlain by the Bursum Formation.[2]
The formation likely correlates with the Panther Seep Formation in the San Andres Mountains.[1][2]
Fossils
editHistory of investigation
editThe formation was first defined by V.C.Kelley and Caswell Silver in 1952.[3] Bachman and Myers criticized its definition in 1975,[1] but it is accepted by Kues and Giles, though they restrict it to the Caballo Mountains.[2]
See also
editReferences
edit- ^ a b c Bachman, G.O.; Myers, D.A. (1975). "The Lead Camp Limestone and its correlatives in south-central New Mexico" (PDF). New Mexico Geological Society Field Conference Guidebook. 26: 105–108. Retrieved 30 July 2020.
- ^ a b c d e 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.
- ^ a b c Kelley, V.C.; Silver, Caswell (1952). "Geology of the Caballo Mountains; with special reference to regional stratigraphy and structure and to mineral resources, including oil and gas". University of New Mexico Publications in Geology. 4.