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Buda Limestone stratigraphic column in Texas. The Buda Limestone is a geological formation in the High Plains and Trans-Pecos regions of West Texas [1] and in southern New Mexico, [2] whose strata date back to the Late Cretaceous. Pterosaur remains are among the fossils that have been recovered from the formation. [3]
Fort Worth Limestone: Cretaceous: Fredericksburg Group/Comanche Peak Limestone: Cretaceous: Fredericksburg Group/Edwards Limestone: Cretaceous: Fredericksburg Group/Goodland Formation: Cretaceous: Fredericksburg Group/Stuart City Formation: Cretaceous: Fredericksburg Group/Walnut Formation: Cretaceous: Fredericksburg Group/Glen Rose Limestone ...
Texas has been the leading state in petroleum production since discovery of the Spindletop oil field in 1901. [11] As of October 2017, the State of Texas (if treated as its own nation) is the 7th largest oil producing nation in the world, with production totaling approximately 3.78 million barrels (600 thousand cubic meters ) per day of oil ...
Anacacho Limestone stratigraphic column in Texas. The Anacacho Limestone is a unit of limestone of Cretaceous (Campanian) age in Texas. Description
The Gunsight Limestone Member is a geologic member in Texas. It preserves fossils. [1] Named in 1919 as the top member of Gunsight formation in Texas, by Frederick B. Plummer. [2] [3] Raymond C. Moore and Plummer assigned the Gunsight limestone to the Graham Formation. [4]
The Edwards Group is a geologic group in Texas. It preserves fossils dating back to the Cretaceous period. A stratigraphic column at the Mount Bonnell Fault location starts with the Lower Cretaceous Trinity Group overlain by the Edwards Group. Upper Cretaceous formations follow, starting with the Del Rio Clay, Buda Limestone, and then the Eagle ...
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The formation consists of up to 300 feet (91 m) [3] of gypsum or anhydrite with a few thin beds of limestone. [3] [2] The formation is found within the Delaware Basin and was deposited after the formation of the Capitan Formation, the fossil reef defining the margins of the Delaware Basin. [4]
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