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″N107°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 |
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]
The 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]
The 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]